[{"data":1,"prerenderedAt":-1},["ShallowReactive",2],{"_public_publisher_byId_454a4c0f-36b8-4ebf-ab13-81feb891f0a9":3,"_public_publication_all{\"sortAscending\":false,\"sortField\":\"updateTime\",\"page\":0,\"size\":10,\"facet\":true,\"searchKey\":\"publisherId:454a4c0f-36b8-4ebf-ab13-81feb891f0a9,\"}":98},{"code":4,"data":5,"meta":24},"SUCCESS",{"id":6,"createTime":7,"updateTime":8,"relativeEntities":9,"slug":10,"properties":11,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":26,"manageAffiliations":35,"indexDatabases":58,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},"454a4c0f-36b8-4ebf-ab13-81feb891f0a9","2023-05-29T10:56:43.185+00:00","2025-11-21T09:49:27.420+00:00",[],"Scottish-Journal-of-Geology",{"country":12,"issn":14,"introduce":16,"eissn":18,"title":20},{"VOID":13},"GB",{"VOID":15},"00369276",{"EN":17},"Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology.",{"VOID":19},"20414951",{"EN":21},"Scottish Journal of Geology","PUBLISHER","PENDING",null,0,[27],{"id":28,"createTime":29,"updateTime":30,"relativeEntities":31,"label":32,"description":34,"parentId":24,"standard":24,"scholarHubFieldId":24},"4cb4a523-c417-4606-9969-2d1fe12ec173","2023-05-29T10:23:59.893+00:00","2023-11-21T08:05:46.044+00:00",[],{"EN":33},"Geology",{},[36,47],{"id":37,"createTime":38,"updateTime":39,"relativeEntities":40,"slug":41,"properties":42,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"url":24,"parentIds":46,"statistic":24},"9239e827-1421-4a94-9142-2fdaa45935db","2023-05-29T12:43:16.011+00:00","2023-12-21T03:49:27.231+00:00",[],"GEOLOGICAL-SOC-PUBL-HOUSE",{"title":43},{"EN":44},"GEOLOGICAL SOC PUBL HOUSE","AFFILIATION",[],{"id":48,"createTime":49,"updateTime":50,"relativeEntities":51,"slug":52,"properties":53,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":56,"url":24,"parentIds":57,"statistic":24},"595cff28-bc2b-4e55-89ce-64629ea2e0c9","2023-05-29T10:31:10.126+00:00","2025-11-21T10:05:17.935+00:00",[],"Geological-Society-of-London",{"title":54},{"EN":55},"Geological Society of London",2,[],[59,78],{"id":60,"indexDatabase":61,"url":73,"indexYears":74,"academicFieldIds":75,"indexDatabaseRanking":77},"b4078cc5-550d-4722-8932-d8c82d09146e",{"id":62,"createTime":63,"updateTime":64,"relativeEntities":65,"label":66,"description":68,"key":70,"publicationTags":71,"standard":24},"3c7051d4-eb7d-4c57-a56b-36fc74c5d1e9","2023-05-22T09:57:18.509+00:00","2025-11-21T10:07:52.274+00:00",[],{"EN":67,"VI":67},"Scopus - Elsevier",{"EN":67,"VI":69},"Cơ sở dữ liệu Scopus thuộc Elsevier","scopus",[72],"SCOPUS","https:\u002F\u002Fwww.scopus.com\u002Fsourceid\u002F26317","1965-2024",[76],"daacc282-927f-40f0-915e-161403c1fcb7","SCOPUS__Q2",{"id":79,"indexDatabase":80,"url":94,"indexYears":24,"academicFieldIds":95,"indexDatabaseRanking":24},"5811fc4c-d220-4e09-9191-bb4c296536bf",{"id":81,"createTime":82,"updateTime":83,"relativeEntities":84,"label":85,"description":87,"key":90,"publicationTags":91,"standard":24},"a4921856-b128-4d9f-8f1f-e80813d3bbd4","2023-05-22T09:59:31.026+00:00","2025-11-21T10:07:52.153+00:00",[],{"EN":86,"VI":86},"ISI\u002FSCIE - Science Citation Index Expanded",{"VI":88,"EN":89},"Cơ sở dữ liệu SCIE","SCIE database","scie",[92,93],"SCIE","ISI","https:\u002F\u002Fmjl.clarivate.com\u002Fsearch-results?issn=0036-9276",[96],"c1bcbdba-82d1-41f4-821c-5a8d86705f7b","https:\u002F\u002Fwww.geolsoc.org.uk\u002Fsjg",{"meta":99,"data":101},{"total":100},"8",[102,400,613,819,1000,1189,1322,1906],{"id":103,"createTime":104,"updateTime":104,"relativeEntities":105,"slug":106,"properties":107,"entityType":119,"verifyStatus":120,"verifyTime":104,"verifyNote":121,"syncStatus":23,"languages":122,"translateLanguages":24,"viewCount":25,"primaryUrl":124,"fullTextUrl":24,"authors":125,"publicationType":177,"publisherRelationship":178,"citationCount":211,"citationInfo":212,"publishDate":214,"publishYear":215,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":216,"isForceReanalyzing":399},"2fed463c-fa29-4b70-8f29-37b5a301a0f2","2024-07-18T22:17:32.778+00:00",[],"Garnet-pyroxenite-xenoliths-and-pyropic-megacrysts-in-Scottish-alkali-basalts",{"mag":108,"keywords":110,"openalex":111,"abstract":113,"title":115,"doi":117},{"VOID":109},"2148917677",{},{"VOID":112},"W2148917677",{"EN":114},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>Pyropic garnet occurs within garnet pyroxenite xenoliths and as discrete crystals in Carboniferous–Permian alkali basaltic tuffs and hypabyssal intrusions. Eight localities are now known from the Midland Valley together with another in the NW Highlands. The xenoliths are inferred to have been derived from minor pyroxenitic intercalations in spinel lherzolite within the lithospheric mantle. Although pyrope crystals at Elie Ness are regarded as high-pressure phenocrysts cognate with the basanitic host, it is indeterminable whether discrete garnets at the other localities are phenocrysts or xenocrystal fragments derived from garnet pyroxenites. All, however, whether phenocrystic, xenocrystic or integral components of pyroxenitic xenoliths, are regarded as cognate in the sense of being products of high-pressure crystallization of late Palaeozoic basanite magmas. Kaersutite, phlogopite, hercynitic spinel, ilmenite and pseudomorphs after orthopyroxene occur as minor components in some of the garnet pyroxenite xenoliths.\u003C\u002Fjats:p>\n          \u003Cjats:p>Mineral compositional data (electron- and ion-microprobe) are presented, with comparisons to xenolith-megacryst suites elsewhere. The garnets have strong similarities with each other and with megacryst populations from alkali basalts outside the U.K. It is concluded that the pyroxenites originally crystallized from basaltic magmas as high-pressure cumulates from depths of >50 km and represent some of the deepest samples from the Scottish lithosphere.\u003C\u002Fjats:p>",{"EN":116},"Garnet pyroxenite xenoliths and pyropic megacrysts in Scottish alkali basalts",{"VOID":118},"10.1144\u002Fsjg39020169","PUBLICATION","VERIFIED","Auto Verify",[123],"EN","https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg39020169",[126,146,162],{"id":127,"sortIndex":25,"researcher":24,"roles":128,"affiliations":129,"properties":141},"f7802b0e-2b9a-4a97-b4bc-232306919a43",[],[130],{"id":131,"sortIndex":25,"affiliation":132,"properties":24},"1a228ab9-9237-4d28-abcc-0285f02b03d9",{"id":133,"createTime":134,"updateTime":135,"relativeEntities":136,"slug":137,"properties":138,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"e3bebc13-94a7-4fca-b638-3dbfc4be91e9","2023-12-14T06:32:35.352+00:00","2024-08-22T06:59:36.099+00:00",[],"School-of-GeoSciences-University-of-Edinburgh-Edinburgh-EH9-3JW-UK",{"title":139},{"VI":140},"School of GeoSciences, University of Edinburgh, Edinburgh EH9 3JW, UK",{"openalex":142,"title":144},{"VOID":143},"A5027492596",{"EN":145},"B. G. J. Upton",{"id":147,"sortIndex":148,"researcher":24,"roles":149,"affiliations":150,"properties":157},"cf86bb8f-3aa3-4173-b268-43b22c3f50dd",1,[],[151],{"id":152,"sortIndex":25,"affiliation":153,"properties":24},"2cf3605a-7d07-459b-9283-603c8b1d0b49",{"id":133,"createTime":134,"updateTime":135,"relativeEntities":154,"slug":137,"properties":155,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},[],{"title":156},{"VI":140},{"openalex":158,"title":160},{"VOID":159},"A5019335871",{"EN":161},"Peder Aspen",{"id":163,"sortIndex":56,"researcher":24,"roles":164,"affiliations":165,"properties":172},"0116d168-c461-44e5-8620-06aeb8057b54",[],[166],{"id":167,"sortIndex":25,"affiliation":168,"properties":24},"e7768272-fc93-4e50-bd5f-8020542d0116",{"id":133,"createTime":134,"updateTime":135,"relativeEntities":169,"slug":137,"properties":170,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},[],{"title":171},{"VI":140},{"openalex":173,"title":175},{"VOID":174},"A5007086120",{"EN":176},"R. W. Hinton","ARTICLE",{"url":24,"publisher":179,"properties":204},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":180,"slug":10,"properties":181,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":187,"manageAffiliations":188,"indexDatabases":189,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":182,"issn":183,"introduce":184,"eissn":185,"title":186},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[190,197],{"id":60,"indexDatabase":191,"url":73,"indexYears":74,"academicFieldIds":196,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":192,"label":193,"description":194,"key":70,"publicationTags":195,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":198,"url":94,"indexYears":24,"academicFieldIds":203,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":199,"label":200,"description":201,"key":90,"publicationTags":202,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":205,"pages":207,"issue":209},{"VOID":206},"39",{"VOID":208},"169-184",{"VOID":210},"2",14,{"total":211,"publishYear":24,"statisticByYear":213},{"2012":148,"2013":148,"2016":56,"2018":56,"2020":148,"2022":148},"2003-11-01",2003,[217,220,223,226,229,232,235,238,241,244,247,250,253,256,259,262,265,268,271,274,277,280,283,286,289,292,295,298,301,304,307,310,313,316,319,323,326,329,332,335,338,341,344,347,350,354,357,360,363,366,369,372,375,378,381,384,387,390,393,396],{"id":24,"text":218,"url":24,"identifiers":219},"10.1180\u002Fminmag.1965.034.268.02",{"doi":218},{"id":24,"text":221,"url":24,"identifiers":222},"10.1144\u002Fsjg20030297",{"doi":221},{"id":24,"text":224,"url":24,"identifiers":225},"10.1093\u002Fpetrology\u002F37.4.785",{"doi":224},{"id":24,"text":227,"url":24,"identifiers":228},"BEESON, M. H. & JACKSON, E. D. 1970. Origin of garnet pyroxenite xenoliths at Salt Lake Crater, Oahu. Fiftieth Anniversary Symposia: Mineralogy and Petrology of the Upper Mantle, Sulfides, Mineralogy and Geochemistry of Non-marine Evaporites. Mineralogical Society of America. Special Paper, 3, 95–112.",{},{"id":24,"text":230,"url":24,"identifiers":231},"10.2475\u002Fajs.269.2.132",{"doi":230},{"id":24,"text":233,"url":24,"identifiers":234},"10.1016\u002F0024-4937(78)90006-3",{"doi":233},{"id":24,"text":236,"url":24,"identifiers":237},"10.1126\u002Fscience.283.5406.1303",{"doi":236},{"id":24,"text":239,"url":24,"identifiers":240},"10.1038\u002F372452a0",{"doi":239},{"id":24,"text":242,"url":24,"identifiers":243},"10.1093\u002Fpetrology\u002F12.1.121",{"doi":242},{"id":24,"text":245,"url":24,"identifiers":246},"CHAPMAN N. A. 1974. Petrology of inclusions from some late Palaeozoic British volcanic rocks. Ph.D. thesis University of Edinburgh UK.",{},{"id":24,"text":248,"url":24,"identifiers":249},"10.1093\u002Fpetrology\u002F17.4.472",{"doi":248},{"id":24,"text":251,"url":24,"identifiers":252},"10.1144\u002Fsjg04030283",{"doi":251},{"id":24,"text":254,"url":24,"identifiers":255},"10.1144\u002Ftransed.13.3.340",{"doi":254},{"id":24,"text":257,"url":24,"identifiers":258},"DICKEY, J. S. 1968. Eclogitic and other inclusions in the Mineral Breccia Member of the Deborah Volcanic Formation at Kakanui, New Zealand. American Mineralogist, 53, 1304–1319.",{},{"id":24,"text":260,"url":24,"identifiers":261},"10.1017\u002FS0016756800030752",{"doi":260},{"id":24,"text":263,"url":24,"identifiers":264},"10.1093\u002Fpetrology\u002F23.4.507",{"doi":263},{"id":24,"text":266,"url":24,"identifiers":267},"10.1007\u002FBF00371878",{"doi":266},{"id":24,"text":269,"url":24,"identifiers":270},"FABRIÉS, J., LORAND, J-P., BODINIER, J-L. & DUPUY, C. 1991. Evolution of the upper mantle beneath the Pyrenees: evidence from orogenic spinel lherzolite massifs. Journal of Petrology, Special Lherzolite issue, 55–76.",{},{"id":24,"text":272,"url":24,"identifiers":273},"10.1144\u002Fsjg06020162",{"doi":272},{"id":24,"text":275,"url":24,"identifiers":276},"10.1016\u002F0012-821X(78)90130-9",{"doi":275},{"id":24,"text":278,"url":24,"identifiers":279},"FRISCH, T. & WRIGHT, J. B. 1971. Chemical composition of high-pressure megacrysts from Nigerian Cenozoic lavas. Neues Jarbuck für Mineralogie, Monatshefte, 7, 289–304.",{},{"id":24,"text":281,"url":24,"identifiers":282},"10.1007\u002FBF00303452",{"doi":281},{"id":24,"text":284,"url":24,"identifiers":285},"10.1016\u002F0012-821X(73)90214-8",{"doi":284},{"id":24,"text":287,"url":24,"identifiers":288},"10.1093\u002Fpetrology\u002F25.1.53",{"doi":287},{"id":24,"text":290,"url":24,"identifiers":291},"10.1016\u002FS0009-2541(96)00127-1",{"doi":290},{"id":24,"text":293,"url":24,"identifiers":294},"10.1016\u002F0009-2541(94)90126-0",{"doi":293},{"id":24,"text":296,"url":24,"identifiers":297},"HEDDLE, M. F. 1901. The Mineralogy of Scotland, 2. D. Douglas, Edinburgh, 47–48.",{},{"id":24,"text":299,"url":24,"identifiers":300},"HEDDLE, M. F. 1895. Geology and mineralogy of Fife. In Millar, A. H. (ed.) Fife: Pictorial and Historical. A. Westwood & Sons, Cupar, Fife, 17–38.",{},{"id":24,"text":302,"url":24,"identifiers":303},"10.1017\u002FS026359330001083X",{"doi":302},{"id":24,"text":305,"url":24,"identifiers":306},"HUNTER, R. H. & UPTON, B. G. J. 1987. The British Isles – a Palaeozoic mantle sample. In Nixon, P. H. (ed.) Mantle Xenoliths, Wiley, New York, 107–118.",{},{"id":24,"text":308,"url":24,"identifiers":309},"10.1093\u002Fpetrology\u002F15.1.1",{"doi":308},{"id":24,"text":311,"url":24,"identifiers":312},"10.1016\u002F0016-7037(78)90092-3",{"doi":311},{"id":24,"text":314,"url":24,"identifiers":315},"10.1016\u002F0016-7037(84)90056-5",{"doi":314},{"id":24,"text":317,"url":24,"identifiers":318},"10.1007\u002Fs004100050437",{"doi":317},{"id":24,"text":320,"url":24,"identifiers":321},"KIRKLEY, M. B., McCALLUM, M. E. & EGGLER, D. H. 1984. Coexisting garnet and spinel in upper mantle xenoliths from Colorado-Wyoming kimberlites. In Kornprobst, J. (ed.) Kimberlites II, The Mantle and Crust-Mantle Relationships. Developments in Petrology, v. II B, Elsevier, Amsterdam, 85–96.",{"doi":322},"10.1016\u002FB978-0-444-42274-3.50014-7",{"id":24,"text":324,"url":24,"identifiers":325},"10.2113\u002Fgssgfbull.III.2.345",{"doi":324},{"id":24,"text":327,"url":24,"identifiers":328},"10.1007\u002FBF00377416",{"doi":327},{"id":24,"text":330,"url":24,"identifiers":331},"10.1007\u002FBF00389414",{"doi":330},{"id":24,"text":333,"url":24,"identifiers":334},"10.1080\u002F00288306.1973.10555233",{"doi":333},{"id":24,"text":336,"url":24,"identifiers":337},"10.1016\u002F0016-7037(92)90195-O",{"doi":336},{"id":24,"text":339,"url":24,"identifiers":340},"10.1016\u002F0009-2541(94)00140-4",{"doi":339},{"id":24,"text":342,"url":24,"identifiers":343},"10.1007\u002FBF00284516",{"doi":342},{"id":24,"text":345,"url":24,"identifiers":346},"MENZIES, M. A. & HALLIDAY, A. N. 1988. Lithospheric mantle domains beneath the Archean and Proterozoic crust of Scotland. Journal of Petrology, Special Lithosphere Issue, 275–302.",{},{"id":24,"text":348,"url":24,"identifiers":349},"MONAGHAN, A. A. & PRINGLE, M. S. 2003. High Precision 40Ar\u002F39Ar Geochronology of Permo–Carboniferous Volcanism in the Midland Valley, Scotland. In Wilson, M. (ed.) Permo–Carboniferous magmatism and rifting. Special Publications, The Geological Society, London, in press.",{},{"id":24,"text":351,"url":24,"identifiers":352},"MOUKADIRI, A. & KORNPROBST, J. 1984. Garnet and\u002For spinel bearing pyroxenites in alkali basalts near Azrou (Middle Atlas, Morocco): mantle derived alumina-rich xenoliths related to the ‘ariegite-grospydite’ trend. In Kornprobst, J. (ed.) Kimberlites II, The Mantle and Crust-Mantle Relationships. Developments in Petrology, v. II B, Elsevier, Amsterdam, 179–190.",{"doi":353},"10.1016\u002FB978-0-444-42274-3.50021-4",{"id":24,"text":355,"url":24,"identifiers":356},"10.1016\u002F0009-2541(94)00147-Z",{"doi":355},{"id":24,"text":358,"url":24,"identifiers":359},"10.1144\u002Fsjg37010027",{"doi":358},{"id":24,"text":361,"url":24,"identifiers":362},"REAY, A. & SPIERA, P. P. 1987. Mantle xenoliths from the New Zealand region. In Nixon, P. H. (ed.) Mantle Xenoliths. John Wiley & Sons Ltd., UK, 347–358.",{},{"id":24,"text":364,"url":24,"identifiers":365},"ROCK N. M. S. 1983. The Permo–Carboniferous camptonite-monchiquite dyke-suite of the Scottish Highlands and Islands: distribution field and petrological aspects. Report of the Institute of Geological Sciences No. 82\u002F14.",{},{"id":24,"text":367,"url":24,"identifiers":368},"SCHULZE, D. J. 1987. Megacrysts in alkali volcanic rocks. In Nixon, P. H. (ed.) Mantle Xenoliths. John Wiley & Sons Ltd., UK, 347–358.",{},{"id":24,"text":370,"url":24,"identifiers":371},"10.1144\u002Fsjg20030315",{"doi":370},{"id":24,"text":373,"url":24,"identifiers":374},"10.1080\u002F08120099408728130",{"doi":373},{"id":24,"text":376,"url":24,"identifiers":377},"10.1093\u002Fpetrology\u002F10.2.332",{"doi":376},{"id":24,"text":379,"url":24,"identifiers":380},"10.1144\u002Fgsjgs.140.1.0105",{"doi":379},{"id":24,"text":382,"url":24,"identifiers":383},"10.1144\u002Fgsjgs.155.5.0813",{"doi":382},{"id":24,"text":385,"url":24,"identifiers":386},"10.1093\u002Fpetroj\u002F40.6.935",{"doi":385},{"id":24,"text":388,"url":24,"identifiers":389},"10.1007\u002Fs004100100282",{"doi":388},{"id":24,"text":391,"url":24,"identifiers":392},"10.1144\u002Ftransglas.25.1.72",{"doi":391},{"id":24,"text":394,"url":24,"identifiers":395},"10.1016\u002F0079-1946(75)90021-X",{"doi":394},{"id":24,"text":397,"url":24,"identifiers":398},"10.1016\u002FS0024-4937(00)00024-4",{"doi":397},false,{"id":401,"createTime":402,"updateTime":402,"relativeEntities":403,"slug":404,"properties":405,"entityType":119,"verifyStatus":120,"verifyTime":402,"verifyNote":121,"syncStatus":23,"languages":417,"translateLanguages":24,"viewCount":25,"primaryUrl":418,"fullTextUrl":24,"authors":419,"publicationType":177,"publisherRelationship":440,"citationCount":473,"citationInfo":474,"publishDate":477,"publishYear":478,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":479,"isForceReanalyzing":399},"9040d909-ec54-406a-8937-2370e4276e1d","2024-09-21T21:54:01.462+00:00",[],"Torridonian-alluvium-and-quicksands",{"mag":406,"keywords":408,"openalex":409,"abstract":411,"title":413,"doi":415},{"VOID":407},"2036587321",{},{"VOID":410},"W2036587321",{"EN":412},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>This paper provides new data on Torridonian alluvium on Raasay, confirming its braided origin and refining its environmental interpretation. Fining-upwards cycles appear to be absent. This may be an important criterion in distinguishing deposits of braided rivers from those due to meandering rivers. A quantitative study reveals a close correlation between grain size and sedimentary structures. With decreasing grain size, the sedimentary structures are broadly arranged in the following order: trough cross-bedding, planar cross-bedding, flat bedding, massive bedding, micro-cross-lamination, lamination.\u003C\u002Fjats:p>\n          \u003Cjats:p>Two types of siltstone sequences are distinguished. The more common type lies between two erosional surfaces and is attributed to deposition in abandoned channels. Its thickness suggests that streams seldom attained a depth of more than one metre in this environment. The second type is attributable to overbank deposition, having an erosional top and a transitional base.\u003C\u002Fjats:p>\n          \u003Cjats:p>Finally, the origin of the ubiquitous Torridonian quicksand structures is considered in the light of experimental work. Previous writers have put forward three possible triggering mechanisms for these bedding disturbances, viz.: springs, earthquakes and current turbulence. Simulation of all three processes produced quicksands in the laboratory but the weight of evidence suggests current turbulence to be the most probable triggering mechanism.\u003C\u002Fjats:p>",{"EN":414},"Torridonian alluvium and quicksands",{"VOID":416},"10.1144\u002Fsjg05040328",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg05040328",[420],{"id":421,"sortIndex":25,"researcher":24,"roles":422,"affiliations":423,"properties":435},"8a589c61-8a5d-4fb5-910d-5fa30f2ed1de",[],[424],{"id":425,"sortIndex":25,"affiliation":426,"properties":24},"fec3df8e-de50-4443-9fc1-c5ec4b9153c1",{"id":427,"createTime":428,"updateTime":429,"relativeEntities":430,"slug":431,"properties":432,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"3bab5cc8-56a4-4302-b0d8-a5887796bd40","2024-01-03T03:44:05.056+00:00","2024-09-21T21:54:01.480+00:00",[],"Department-of-Geology-Imperial-College-London",{"title":433},{"VI":434},"Department of Geology, Imperial College, London",{"openalex":436,"title":438},{"VOID":437},"A5006381872",{"EN":439},"Richard C. Selley",{"url":24,"publisher":441,"properties":466},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":442,"slug":10,"properties":443,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":449,"manageAffiliations":450,"indexDatabases":451,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":444,"issn":445,"introduce":446,"eissn":447,"title":448},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[452,459],{"id":60,"indexDatabase":453,"url":73,"indexYears":74,"academicFieldIds":458,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":454,"label":455,"description":456,"key":70,"publicationTags":457,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":460,"url":94,"indexYears":24,"academicFieldIds":465,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":461,"label":462,"description":463,"key":90,"publicationTags":464,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":467,"pages":469,"issue":471},{"VOID":468},"5",{"VOID":470},"328-346",{"VOID":472},"4",59,{"total":473,"publishYear":24,"statisticByYear":475},{"2012":148,"2014":56,"2015":148,"2016":476,"2017":148,"2021":148,"2022":148,"2023":148},3,"1969-12-01",1969,[480,483,486,489,492,495,498,501,504,507,510,513,516,519,522,525,528,531,534,537,540,543,546,549,552,555,558,561,565,568,571,574,577,580,583,586,589,592,595,598,601,604,607,610],{"id":24,"text":481,"url":24,"identifiers":482},"10.1111\u002Fj.1365-3091.1964.tb00459.x",{"doi":481},{"id":24,"text":484,"url":24,"identifiers":485},"10.1002\u002Fgj.3350040201",{"doi":484},{"id":24,"text":487,"url":24,"identifiers":488},"ALLEN J. R. L. 1965b. Upper Old Red sand palaeogeography in S. Wales and the Welsh Borderland. J. sedim. Petrol. 35, 167–196.",{},{"id":24,"text":490,"url":24,"identifiers":491},"10.1111\u002Fj.1365-3091.1965.tb01561.x",{"doi":490},{"id":24,"text":493,"url":24,"identifiers":494},"BAGNOLD R. A. 1941. Physics of Blown Sands and Desert Dunes. London.",{},{"id":24,"text":496,"url":24,"identifiers":497},"BARRATT P. J. 1966. Effects of the 1964 Alaskan earthquake on some shallow water sediments in Prince William Sound, S.E. Alaska. J. sedim. Petrol. 36, 992–1006.",{},{"id":24,"text":499,"url":24,"identifiers":500},"10.1017\u002FS0016756800060581",{"doi":499},{"id":24,"text":502,"url":24,"identifiers":503},"DAVIDSON C. 1936. Great Earthquakes. London.",{},{"id":24,"text":505,"url":24,"identifiers":506},"10.1111\u002Fj.1365-3091.1962.tb00453.x",{"doi":505},{"id":24,"text":508,"url":24,"identifiers":509},"FREUNDLICH H., JULIUSBERGER J. 1935. Quicksand as a thixotropic system. Trans. Faraday Soc. 3, 5.",{},{"id":24,"text":511,"url":24,"identifiers":512},"GILL W. D., KUENEN P. H. 1958. Sand volcanoes and slumps in the Carboniferous of County Clare, Ireland. Q. Jl geol. Soc. Lond. 118, 441–460.",{},{"id":24,"text":514,"url":24,"identifiers":515},"10.5962\u002Fbhl.title.15101",{"doi":514},{"id":24,"text":517,"url":24,"identifiers":518},"10.1144\u002Fsjg03020181",{"doi":517},{"id":24,"text":520,"url":24,"identifiers":521},"GRAF-PETERSON P. 1967. Intraformational deformations and pore-water hydrodynamics. Preprint Seventh Int. Sedimentological Congr, Great Britain 1967.",{},{"id":24,"text":523,"url":24,"identifiers":524},"HARMS J. C., FAHNESTOCK R. K. 1965. Stratification, Bed Forms and Flow Phenomena (with an example from the Rio Grande). Spec. Publs. Soc. econ. Paleont. Miner., 12, 84–115.",{},{"id":24,"text":526,"url":24,"identifiers":527},"HOBBS W. H. 1907. Earthquakes, an introduction to Seismic Geology. New York.",{},{"id":24,"text":529,"url":24,"identifiers":530},"JONES G. P. 1962. Deformed cross-stratification in Cretaceous Bima sandstone, Nigeria, J. sediment. Petrol. 32, 231–240.",{},{"id":24,"text":532,"url":24,"identifiers":533},"KENDAL P. 1922. The physiography of coal swamps. 90th Rep. Brit. Assn. Advmt. Sci., 49–78.",{},{"id":24,"text":535,"url":24,"identifiers":536},"LEOPOLD L. B., WOLMAN M. G. 1957. River channel patterns: Braided, Meandering and Straight. Prof. Paps. U.S. geol. Surv. 282-B, 39–85.",{},{"id":24,"text":538,"url":24,"identifiers":539},"McKEE E. D., REYNOLDS M. A., BAKER C. H. 1962. Experiments on intraformational recumbent folds in cross-bedded sand. Prof. Paps. U.S. geol. Surv. 450 D, 155–160.",{},{"id":24,"text":541,"url":24,"identifiers":542},"10.1306\u002F74D717B2-2B21-11D7-8648000102C1865D",{"doi":541},{"id":24,"text":544,"url":24,"identifiers":545},"OULIANOFF M. N. 1958. Géologie: sedimentologie et géophysique. C. R. Acad. Sci. L.247, 313–315.",{},{"id":24,"text":547,"url":24,"identifiers":548},"PEACH B. N., HORNE J., GUNN W., CLOUGH C. T., HINXMAN L. W., TEALL J. J. H. 1907. The geological structure of the north-west highlands of Scotland. Mem. geol. Surv. U.K.",{},{"id":24,"text":550,"url":24,"identifiers":551},"PLUMMER F. L., DORE S. M. 1940. Soil Mechanics and Foundations. New York.",{},{"id":24,"text":553,"url":24,"identifiers":554},"10.1007\u002F978-3-662-01020-4",{"doi":553},{"id":24,"text":556,"url":24,"identifiers":557},"RAYNER D. H. 1967. The Stratigraphy of the British Isles. Cambridge.",{},{"id":24,"text":559,"url":24,"identifiers":560},"RETTGER R. 1935. Experiments in soft rock deformation. Bull. Amer. Assoc. petrol. geol. 19, 271.",{},{"id":24,"text":562,"url":24,"identifiers":563},"SELLEY R. C. 1964. The penecontemporaneous deformation of heavy mineral bands in the Torridonian Sandstone of N.W. Scotland. In , Van Straaten L.M.J.U., editor, Deltaic and Shallow Marine Deposits. Amsterdam. 362–367.",{"doi":564},"10.1016\u002FS0070-4571(08)70509-0",{"id":24,"text":566,"url":24,"identifiers":567},"10.1306\u002F74D7127B-2B21-11D7-8648000102C1865D",{"doi":566},{"id":24,"text":569,"url":24,"identifiers":570},"10.1017\u002FS0016756800053632",{"doi":569},{"id":24,"text":572,"url":24,"identifiers":573},"10.1016\u002FS0016-7878(66)80036-6",{"doi":572},{"id":24,"text":575,"url":24,"identifiers":576},"SELLEY R. C., SHEARMAN D. J. 1962. Experimental production of sedimentary structures in quick-sands. Proc. geol. Soc. Lond. 1599, 101–102.",{},{"id":24,"text":578,"url":24,"identifiers":579},"10.1017\u002FS0016756800055175",{"doi":578},{"id":24,"text":581,"url":24,"identifiers":582},"SHANTSTER Y. V. 1951. The flatland fluvial alluvia of the temperate zone and its significance for the perception of the structural and formative regularities of alluvial rivers. Tr. Inst. Geol. Nauk, Akad. Nauk S.S.S.R. Geol. Ser. 135, 1–137.",{},{"id":24,"text":584,"url":24,"identifiers":585},"10.1002\u002Fgj.3350030111",{"doi":584},{"id":24,"text":587,"url":24,"identifiers":588},"10.1017\u002FS0016756800055151",{"doi":587},{"id":24,"text":590,"url":24,"identifiers":591},"10.1017\u002FS0016756800054030",{"doi":590},{"id":24,"text":593,"url":24,"identifiers":594},"10.1017\u002FS0016756800061227",{"doi":593},{"id":24,"text":596,"url":24,"identifiers":597},"10.1016\u002FS0016-7878(64)80033-X",{"doi":596},{"id":24,"text":599,"url":24,"identifiers":600},"TERZAGHI K., PECK R. 1960. Soil Mechanics in Engineering Practice. New York.",{},{"id":24,"text":602,"url":24,"identifiers":603},"TOLMAN C. F. 1937. Groundwater. New York.",{},{"id":24,"text":605,"url":24,"identifiers":606},"VISHER G. S. 1965. Fluvial processes as interpreted from ancient and recent fluviatile deposits. Spec. Publs. Soc. econ. Paleont. Miner. 12, 116–132.",{},{"id":24,"text":608,"url":24,"identifiers":609},"10.1038\u002F2091303a0",{"doi":608},{"id":24,"text":611,"url":24,"identifiers":612},"WILLIAMS G. E. 1966b. Planar cross-stratification formed by the lateral migration of shallow streams. J. sedim. Petrol. 36, 742–746.",{},{"id":614,"createTime":615,"updateTime":615,"relativeEntities":616,"slug":617,"properties":618,"entityType":119,"verifyStatus":120,"verifyTime":615,"verifyNote":121,"syncStatus":23,"languages":630,"translateLanguages":24,"viewCount":25,"primaryUrl":631,"fullTextUrl":24,"authors":632,"publicationType":177,"publisherRelationship":690,"citationCount":723,"citationInfo":724,"publishDate":726,"publishYear":727,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":728,"isForceReanalyzing":399},"e2c7759e-a6ae-4b7b-b452-d06d2944592f","2024-09-19T20:30:28.227+00:00",[],"The-Geikie-igneous-centre-west-of-Lewis-its-structure-and-influence-on-Tertiary-geology",{"mag":619,"keywords":621,"openalex":622,"abstract":624,"title":626,"doi":628},{"VOID":620},"2142950244",{},{"VOID":623},"W2142950244",{"EN":625},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>The Geikie igneous centre is identified from a large positive gravity anomaly to the west of Lewis. The anomaly is satisfied by a simple two cylinder model with a maximum diameter of 26 km. The centre is covered by Palaeocene basalts which are domed and radially disposed around it. The centre occurs near the apex of a topographic bulge on the slope west of Scotland which overlies thinned crust. The intrusion has had a marked influence on the Tertiary development of the area, principally because it deflected faulting\u002Fflexuring associated with Eocene subsidence of the Rockall Trough to a zone seaward of the intrusion. Subsequent subsidence of the basalt and overlying Tertiary sediment wedge has been hinged at the transition between normal and thinned crust to the east of the centre. The curved bathymetric Geikie Escarpment is not faulted, but is an eroded feature cut into Oligocene sediments on this subsiding wedge.\u003C\u002Fjats:p>",{"EN":627},"The Geikie igneous centre, west of Lewis: its structure and influence on Tertiary geology",{"VOID":629},"10.1144\u002Fsjg25030339",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg25030339",[633,654,673],{"id":634,"sortIndex":25,"researcher":24,"roles":635,"affiliations":636,"properties":647},"c718708f-9292-457b-94f7-3511a5402059",[],[637],{"id":638,"sortIndex":25,"affiliation":639,"properties":24},"6cac2936-c367-4f19-b0bd-59ee0ba03cc4",{"id":640,"createTime":641,"updateTime":641,"relativeEntities":642,"slug":643,"properties":644,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"50a1ebab-7181-412f-99ab-86ce8831d0ba","2024-09-19T20:30:26.031+00:00",[],"British-Geological-Survey-Murchison-House-West-Mains-Road-Edinburgh-EH9-3LA-",{"title":645},{"EN":646},"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA,",{"openalex":648,"orcid":650,"title":652},{"VOID":649},"A5102981989",{"VOID":651},"https:\u002F\u002Forcid.org\u002F0009-0006-4156-8964",{"EN":653},"D. Evans",{"id":655,"sortIndex":56,"researcher":24,"roles":656,"affiliations":657,"properties":668},"9d3b60dc-bb6c-4ae2-9047-1788c1c4e8af",[],[658],{"id":659,"sortIndex":25,"affiliation":660,"properties":24},"1caedd71-4bcf-4c18-9f96-2206bc370ad5",{"id":661,"createTime":662,"updateTime":662,"relativeEntities":663,"slug":664,"properties":665,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"9bcffd6d-7acc-485b-a5d9-c62d19b840ac","2024-09-19T20:30:28.256+00:00",[],"British-Geological-Survey-19-Grange-Terrace-Edinburgh-EH9-2LF",{"title":666},{"EN":667},"British Geological Survey, 19 Grange Terrace, Edinburgh EH9 2LF",{"openalex":669,"title":671},{"VOID":670},"A5051794158",{"EN":672},"K. Hitchen",{"id":674,"sortIndex":148,"researcher":24,"roles":675,"affiliations":676,"properties":683},"6db3c09c-e03f-4b33-99ed-156e0db992ed",[],[677],{"id":678,"sortIndex":25,"affiliation":679,"properties":24},"431a613e-5aab-440e-a211-8034aaf22ae6",{"id":640,"createTime":641,"updateTime":641,"relativeEntities":680,"slug":643,"properties":681,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},[],{"title":682},{"EN":646},{"openalex":684,"orcid":686,"title":688},{"VOID":685},"A5045794018",{"VOID":687},"https:\u002F\u002Forcid.org\u002F0000-0002-7755-0022",{"EN":689},"Douglas A. Abraham",{"url":24,"publisher":691,"properties":716},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":692,"slug":10,"properties":693,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":699,"manageAffiliations":700,"indexDatabases":701,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":694,"issn":695,"introduce":696,"eissn":697,"title":698},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[702,709],{"id":60,"indexDatabase":703,"url":73,"indexYears":74,"academicFieldIds":708,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":704,"label":705,"description":706,"key":70,"publicationTags":707,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":710,"url":94,"indexYears":24,"academicFieldIds":715,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":711,"label":712,"description":713,"key":90,"publicationTags":714,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":717,"pages":719,"issue":721},{"VOID":718},"25",{"VOID":720},"339-352",{"VOID":722},"3",22,{"total":723,"publishYear":24,"statisticByYear":725},{"2012":148},"1989-03-01",1989,[729,732,735,738,741,744,747,750,753,756,759,762,765,768,771,774,777,780,783,786,789,792,795,798,801,804,807,810,813,816],{"id":24,"text":730,"url":24,"identifiers":731},"ABRAHAM D. A. 1988. Geikie, 58°N–10°W, Bouguer Gravity Anomaly, 1:250 000 Map Series, British Geological Survey.",{},{"id":24,"text":733,"url":24,"identifiers":734},"ABRAHAM D. A. RITCHIE J. D. (in prep.) The Darwin Complex a Tertiary igneous centre in the Northern Rockall Trough.",{},{"id":24,"text":736,"url":24,"identifiers":737},"10.1016\u002F0040-1951(79)90046-5",{"doi":736},{"id":24,"text":739,"url":24,"identifiers":740},"10.1144\u002Fgsjgs.144.1.0017",{"doi":739},{"id":24,"text":742,"url":24,"identifiers":743},"10.1016\u002F0025-3227(80)90122-X",{"doi":742},{"id":24,"text":745,"url":24,"identifiers":746},"EVANS D. 1985. Tiree, 56°N–08°W, Solid Geology, 1:250 000 Map Series, British Geological Survey.",{},{"id":24,"text":748,"url":24,"identifiers":749},"EVANS D. HITCHEN K. ABRAHAM D. A. (in press). Geikie 58°N–10°W Solid Geology 1:250 000 Map Series British Geological Survey .",{},{"id":24,"text":751,"url":24,"identifiers":752},"EVANS D. HITCHEN K. (in press). Lewis 58°N–08°W Solid Geology 1:250 000 Map Series British Geological Survey .",{},{"id":24,"text":754,"url":24,"identifiers":755},"EVANS D., McELVANNEY E. P. (in press). Geikie, 58°N–10°W, Quaternary Geology, 1:250 000 Map Series, British Geological Survey.",{},{"id":24,"text":757,"url":24,"identifiers":758},"EVANS D. STRACHAN P. (in press). Geikie 58°N–10°W Sea Bed Sediments 1:250 000 Map Series British Geological Survey .",{},{"id":24,"text":760,"url":24,"identifiers":761},"10.1144\u002Fgsjgs.141.3.0555",{"doi":760},{"id":24,"text":763,"url":24,"identifiers":764},"HARDING R. R., MERRIMAN R. J., NANCARROW P. H. A. 1984. St Kilda: an illustrated account of the geology. Rep. Br. Geol. Surv., 16, No. 7.",{},{"id":24,"text":766,"url":24,"identifiers":767},"HIMSWORTH E. M. 1973. Marine geophysical studies between north-west Scotland and the Faeroe Plateau. Univ. Durham PhD thesis (unpubl.).",{},{"id":24,"text":769,"url":24,"identifiers":770},"JONES E. J. W. 1981. Seismic refraction shooting on the continental margin west of the Outer Hebrides, north-west Scotland. J. Geophys. Res., 86, 11, 553–74.",{},{"id":24,"text":772,"url":24,"identifiers":773},"JONES E. J. W., PERRY R. G., WILD J. L. 1986. Geology of the Hebridean margin of the Rockall Trough. Proc. R. Soc. Edinb., 88B, 27–51.",{},{"id":24,"text":775,"url":24,"identifiers":776},"10.1016\u002F0025-3227(87)90005-3",{"doi":775},{"id":24,"text":778,"url":24,"identifiers":779},"MASSON D. G., KIDD R. B. 1986. Revised Tertiary seismic stratigraphy of the southern Rockall Trough. In , Ruddiman W. F., Kidd R. B., Thomas E., et al.. Init. Rep. Deep Sea Drilling Project, 94, 1117–26.",{},{"id":24,"text":781,"url":24,"identifiers":782},"10.1144\u002Fsjg11030179",{"doi":781},{"id":24,"text":784,"url":24,"identifiers":785},"10.1016\u002F0012-821X(81)90060-1",{"doi":784},{"id":24,"text":787,"url":24,"identifiers":788},"10.1007\u002F978-1-4613-3485-9_27",{"doi":787},{"id":24,"text":790,"url":24,"identifiers":791},"MUSSETT A. E., DAGLEY P., SKELHORN R. R. 1988. Time and duration of activity in the British Tertiary Igneous Province. In , Morton A. C., Parson L. M. (eds) Early Tertiary Volcanism and the opening of the NE Atlantic, Spec. Publ. Geol. Soc. Lond., 39, 337–48.",{},{"id":24,"text":793,"url":24,"identifiers":794},"10.1016\u002F0025-3227(87)90027-2",{"doi":793},{"id":24,"text":796,"url":24,"identifiers":797},"ROBERTS D. G. 1975. Marine geology of the Rockall Plateau and Trough. Philos. Trans. R. Soc. Lond., 278A, 477–509.",{},{"id":24,"text":799,"url":24,"identifiers":800},"10.1038\u002F332632a0",{"doi":799},{"id":24,"text":802,"url":24,"identifiers":803},"ROBERTS D. G., HUNTER P. M., LAUGHTON A. S. 1977. Bathymetry of the northeast Atlantic, sheet 2: Continental margin around the British Isles. Institute of Oceanographic Sciences.",{},{"id":24,"text":805,"url":24,"identifiers":806},"10.1144\u002Fsjg25010005",{"doi":805},{"id":24,"text":808,"url":24,"identifiers":809},"10.1038\u002F276420a0",{"doi":808},{"id":24,"text":811,"url":24,"identifiers":812},"STOKER M. S., HITCHEN K. 1988. Sula Sgeir, 59°N–08°W, Solid Geology, 1:250 000 Map Series, British Geological Survey.",{},{"id":24,"text":814,"url":24,"identifiers":815},"STOKER M. S., MORTON A. C., EVANS D., HUGHES M. J., HARLAND R., GRAHAM D. K. 1988. Early Tertiary basalts and tuffaceous sandstones from the Hebrides Shelf and Wyville-Thomson Ridge, NE Atlantic. In , Morton A. C., Parson L. M. (eds), Early Tertiary Volcanism and the opening of the NE Atlantic, Spec. Publ. Geol. Soc. Lond. 39, 271–82.",{},{"id":24,"text":817,"url":24,"identifiers":818},"WOOD M. V., HALL J., VAN HOORN B. 1987. Post-Mesozoic differential subsidence in the northeast Rockall Trough related to volcanicity and sedimentation. In , Brooks J., Glennie K. (eds), Petroleum Geology of North West Europe, 677–85, Graham and Trotman.",{},{"id":820,"createTime":821,"updateTime":821,"relativeEntities":822,"slug":823,"properties":824,"entityType":119,"verifyStatus":120,"verifyTime":821,"verifyNote":121,"syncStatus":23,"languages":836,"translateLanguages":24,"viewCount":25,"primaryUrl":837,"fullTextUrl":24,"authors":838,"publicationType":177,"publisherRelationship":856,"citationCount":888,"citationInfo":889,"publishDate":891,"publishYear":892,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":893,"isForceReanalyzing":399},"3faf6df1-a907-47cc-bd06-ee53c76d35a1","2024-09-19T20:30:26.013+00:00",[],"Pleistocene-ice-proximal-glaciomarine-sediments-in-boreholes-from-the-Hebrides-Shelf-and-Wyville-Thomson-Ridge-NW-UK-Continental-Shelf",{"mag":825,"keywords":827,"openalex":828,"abstract":830,"title":832,"doi":834},{"VOID":826},"2073996751",{},{"VOID":829},"W2073996751",{"EN":831},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>Pleistocene sediments recovered in boreholes from the Hebrides Shelf and Wyville–Thomson Ridge indicate ice-proximal glaciomarine deposition in an outer shelf setting. The sediments are predominantly diamicts and in vertical profile display a general upward-fining trend. The lower part of the succession is characterised by a coarse, crudely stratified-to-massive, clast and matrix-supported diamict assemblage which is interpreted as an amalgamated sequence of debris flows. The upper part consists of finer, massive, matrix-supported diamicts deposited mainly from suspension but with a subsidiary input of ice-rafted material. Thin interbedded lag gravels and sandy sediment gravity flows form a minor component of the succession. This kind of succession is usually associated with a stationary or slowly retreating tidewater ice margin. The morphology of the outer shelf is characterised by a relict glaciated terrain; the sedimentary succession suggests that this is of submarine origin. These data indicate that at some time during the Pleistocene an ice-sheet extended out to the edge of the northern Hebrides Shelf and partly onto the Wyville-Thomson Ridge. The age of this glaciation is unknown but probably pre-dates the last Scottish ice-sheet (Late Devensian\u002FLate Weichselian)\u003C\u002Fjats:p>",{"EN":833},"Pleistocene ice-proximal glaciomarine sediments in boreholes from the Hebrides Shelf and Wyville-Thomson Ridge, NW UK Continental Shelf",{"VOID":835},"10.1144\u002Fsjg24030249",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg24030249",[839],{"id":840,"sortIndex":25,"researcher":24,"roles":841,"affiliations":842,"properties":849},"37ab63e5-96e2-42a2-906f-f98df92fe154",[],[843],{"id":844,"sortIndex":25,"affiliation":845,"properties":24},"d2cf22ba-870d-43eb-aaf7-bcb9d76586c5",{"id":640,"createTime":641,"updateTime":641,"relativeEntities":846,"slug":643,"properties":847,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},[],{"title":848},{"EN":646},{"openalex":850,"orcid":852,"title":854},{"VOID":851},"A5060615194",{"VOID":853},"https:\u002F\u002Forcid.org\u002F0000-0002-5314-0950",{"EN":855},"Martyn S. Stoker",{"url":24,"publisher":857,"properties":882},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":858,"slug":10,"properties":859,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":865,"manageAffiliations":866,"indexDatabases":867,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":860,"issn":861,"introduce":862,"eissn":863,"title":864},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[868,875],{"id":60,"indexDatabase":869,"url":73,"indexYears":74,"academicFieldIds":874,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":870,"label":871,"description":872,"key":70,"publicationTags":873,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":876,"url":94,"indexYears":24,"academicFieldIds":881,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":877,"label":878,"description":879,"key":90,"publicationTags":880,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":883,"pages":885,"issue":887},{"VOID":884},"24",{"VOID":886},"249-262",{"VOID":722},17,{"total":888,"publishYear":24,"statisticByYear":890},{"2013":148,"2017":148,"2020":148},"1988-03-01",1988,[894,897,900,903,906,909,912,915,918,921,924,927,930,933,936,939,942,945,948,951,954,957,960,963,967,970,973,976,979,982,985,988,991,994,997],{"id":24,"text":895,"url":24,"identifiers":896},"10.1111\u002Fj.1502-3885.1979.tb00788.x",{"doi":895},{"id":24,"text":898,"url":24,"identifiers":899},"10.1144\u002Fgsjgs.144.1.0043",{"doi":898},{"id":24,"text":901,"url":24,"identifiers":902},"10.1017\u002FS0016756800028053",{"doi":901},{"id":24,"text":904,"url":24,"identifiers":905},"DALE B. 1985. Dinoflagellate cyst analysis of Upper Quaternary sediments in core GIK 15530–4 from the Skagerrak. Norsk Geol. Tidsskr. 65, 97–102.",{},{"id":24,"text":907,"url":24,"identifiers":908},"DREIMANIS A. 1976. Tills: their origin and properties. In Legget R. F. (ed) Glacial Till Royal Society of Canada Spec. Publ. No. 12 11–49.",{},{"id":24,"text":910,"url":24,"identifiers":911},"10.1016\u002F0031-0182(85)90079-3",{"doi":910},{"id":24,"text":913,"url":24,"identifiers":914},"EVANS D. (in press). Lewis (58N 8W) Quaternary Geology 1:250 000 Offshore Map Series British Geological Survey.",{},{"id":24,"text":916,"url":24,"identifiers":917},"10.1130\u002F0091-7613(1984)12\u003C359:GSOTIO>2.0.CO;2",{"doi":916},{"id":24,"text":919,"url":24,"identifiers":920},"10.1016\u002F0031-0182(85)90080-X",{"doi":919},{"id":24,"text":922,"url":24,"identifiers":923},"EYLES N., MIALL A. D. 1984. Glacial facies models. In , Walker R. G. (ed), Facies Models Geoscience Canada Reprint Series, Geologists Association of Canada, Toronto 15–38.",{},{"id":24,"text":925,"url":24,"identifiers":926},"10.1111\u002Fj.1365-3091.1983.tb00679.x",{"doi":925},{"id":24,"text":928,"url":24,"identifiers":929},"FRAKES L. A. 1978. Diamictite. In , Fairbridge R. W., Bourgeois J. (eds), The encyclopedia of sedimentology, 262–3, Dowden and Ross, Stroudsberg, Pa.",{},{"id":24,"text":931,"url":24,"identifiers":932},"10.1016\u002F0012-8252(84)90023-0",{"doi":931},{"id":24,"text":934,"url":24,"identifiers":935},"10.1111\u002Fj.1469-8137.1988.tb00210.x",{"doi":934},{"id":24,"text":937,"url":24,"identifiers":938},"10.1144\u002Ftransed.15.1.214",{"doi":937},{"id":24,"text":940,"url":24,"identifiers":941},"KING L. H., FADER G. B. J. 1986. Wisconsinan glaciation of the Atlantic continental shelf of southeast Canada. Bull. Geol. Surv. Can. 363, 72.",{},{"id":24,"text":943,"url":24,"identifiers":944},"KING L. H., MACLEAN B., DRAPEAU G. 1972. The Scotian Shelf submarine endmoraine complex. Int. Geol. Congr. XXIV, Canada, 237–49.",{},{"id":24,"text":946,"url":24,"identifiers":947},"KING L. H. ROKOENGEN K. GUNLEIKSRUD T. 1987. Quaternary seismostratigraphy of the mid Norwegian shelf 65°–67° 30′ N.—A till tongue stratigraphy . IKU publ. no. 114 58pp.",{},{"id":24,"text":949,"url":24,"identifiers":950},"LOWE D. R. 1982. Sediment gravity flows: ii. Depositional models with special reference to the deposits of high-density turbidity currents. J. Sed. Pet. 52, 279–97.",{},{"id":24,"text":952,"url":24,"identifiers":953},"MCCABE A. M., DARDIS G. F., HANVEY P. M. 1984. Sedimentology of a late Pleistocene submarine-moraine complex, County Down, Northern Ireland. J. Sed. Pet. 54, 716–30.",{},{"id":24,"text":955,"url":24,"identifiers":956},"10.1016\u002F0033-5894(85)90005-5",{"doi":955},{"id":24,"text":958,"url":24,"identifiers":959},"OWEN D. E. 1987. Commentary: Usage of stratigraphic terminology in papers, illustrations, and talks. J. Sed. Pet. 57, 363–72.",{},{"id":24,"text":961,"url":24,"identifiers":962},"10.3189\u002F172756481794352306",{"doi":961},{"id":24,"text":964,"url":24,"identifiers":965},"POWELL R. D. 1983. Glacial marine sedimentation processes and lithofacies of temperate tidewater glaciers, Glacier Bay, Alaska. In , Molnia B. F. (ed), Glacial Marine Sedimentation, 185–232, Plenum, New York.",{"doi":966},"10.1007\u002F978-1-4613-3793-5_4",{"id":24,"text":968,"url":24,"identifiers":969},"10.1016\u002F0025-3227(84)90194-4",{"doi":968},{"id":24,"text":971,"url":24,"identifiers":972},"10.1002\u002Fjqs.3390020105",{"doi":971},{"id":24,"text":974,"url":24,"identifiers":975},"STOKER M. S. (in press). Sula Sgeir (59N 8W) Quaternary Geology 1:250 000 Offshore Map Series British Geological Survey.",{},{"id":24,"text":977,"url":24,"identifiers":978},"10.1111\u002Fj.1502-3885.1985.tb00920.x",{"doi":977},{"id":24,"text":980,"url":24,"identifiers":981},"10.1002\u002Fjqs.3390020202",{"doi":980},{"id":24,"text":983,"url":24,"identifiers":984},"10.1016\u002FS0016-7878(87)80020-2",{"doi":983},{"id":24,"text":986,"url":24,"identifiers":987},"STOKER M. S. LONG D. FYFE J. A. 1985. A revised Quaternary stratigraphy for the central North Sea. Rep. Brit. Geol. Surv. No. 17\u002F2.",{},{"id":24,"text":989,"url":24,"identifiers":990},"10.1144\u002Fsjg23030251",{"doi":989},{"id":24,"text":992,"url":24,"identifiers":993},"10.1038\u002F309701a0",{"doi":992},{"id":24,"text":995,"url":24,"identifiers":996},"VAIL P. R., MITCHUM R. M., TODD R. G., WIDMIER J. M., THOMSON S., SANGREE J. B., BUBB J. N., HATLELID W. G. 1977. Seismic stratigraphy and global changes in sea level. In , Payton C. E. (ed), Seismic Stratigraphy—Applications to Hydrocarbon Exploration, Mem. Am. Assoc. Pet. Geol. 26, 49–212.",{},{"id":24,"text":998,"url":24,"identifiers":999},"10.1130\u002F0016-7606(1975)86\u003C737:GFMFRC>2.0.CO;2",{"doi":998},{"id":1001,"createTime":1002,"updateTime":1002,"relativeEntities":1003,"slug":1004,"properties":1005,"entityType":119,"verifyStatus":120,"verifyTime":1002,"verifyNote":121,"syncStatus":23,"languages":1017,"translateLanguages":24,"viewCount":25,"primaryUrl":1018,"fullTextUrl":24,"authors":1019,"publicationType":177,"publisherRelationship":1061,"citationCount":1093,"citationInfo":1094,"publishDate":1096,"publishYear":1097,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1098,"isForceReanalyzing":399},"7ca59f3d-fc4b-4dbb-b6c9-e2eb39d04dd1","2024-09-19T20:30:25.782+00:00",[],"Photographic-evidence-for-slope-current-activity-Hebrides-Slope-NE-Atlantic-Ocean",{"mag":1006,"keywords":1008,"openalex":1009,"abstract":1011,"title":1013,"doi":1015},{"VOID":1007},"2035026832",{},{"VOID":1010},"W2035026832",{"EN":1012},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>\n            Evidence from sea-bed photographs and current-meter data from the Hebrides Slope, indicates that there is a slope-current flowing northward along the bathymetric contours in water depths of 500–1100 m. Structures identified from photographs include: asymmetric linguoid ripples, scours, crag-and-tail structures and current-induced smoothing of the seabed in fine- to medium-grained contourite sands. Bioturbated hemipelagite muds are characterized by populations of the brittle-star\n            \u003Cjats:italic>Ophiocten.\u003C\u002Fjats:italic>\n            The densities of these decrease with increased current activity, suggesting that the organism is sensitive to stronger flows. Current-meter data reveal peak flows of 15–25 cm s\n            \u003Cjats:sup>−1\u003C\u002Fjats:sup>\n            at depths of 1035 m and 457 m, in a north-north-easterly direction, with little depth stratification through the water column, but with fluctuations in velocity and possible tidal oscillation. The current is probably of Eastern North Atlantic Water origin, flowing northwards along the eastern margins of the Rockall Trough.\n          \u003C\u002Fjats:p>",{"EN":1014},"Photographic evidence for slope-current activity, Hebrides Slope, NE Atlantic Ocean",{"VOID":1016},"10.1144\u002Fsjg31020107",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg31020107",[1020,1042],{"id":1021,"sortIndex":25,"researcher":24,"roles":1022,"affiliations":1023,"properties":1035},"ec9c3f8e-1a39-4afb-b4da-5e3aac636901",[],[1024],{"id":1025,"sortIndex":25,"affiliation":1026,"properties":24},"48155cdf-9f2e-4b0a-8ad7-82b87ee42e23",{"id":1027,"createTime":1028,"updateTime":1029,"relativeEntities":1030,"slug":1031,"properties":1032,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"068cafec-320c-48a5-b624-80c2ce032ffe","2024-09-19T20:30:25.798+00:00","2025-06-11T19:37:02.106+00:00",[],"British-Geological-Survey-Marine-Geology-Murchison-House-West-Mains-Road-Edinburgh-EH9-3LA-Southampton-University-Department-of-Geology-Highfield-Southampton-S09-5NH",{"title":1033},{"EN":1034},"British Geological Survey, Marine Geology, Murchison House, West Mains Road, Edinburgh EH9 3LA\u002FSouthampton University, Department of Geology, Highfield, Southampton S09 5NH",{"openalex":1036,"orcid":1038,"title":1040},{"VOID":1037},"A5067109037",{"VOID":1039},"https:\u002F\u002Forcid.org\u002F0000-0002-4617-2209",{"EN":1041},"John Howe",{"id":1043,"sortIndex":148,"researcher":24,"roles":1044,"affiliations":1045,"properties":1056},"764199ec-9aeb-4f70-b8b2-08111749facc",[],[1046],{"id":1047,"sortIndex":25,"affiliation":1048,"properties":24},"289bdc67-24bc-4b7c-8b46-92696eb8c1be",{"id":1049,"createTime":1050,"updateTime":1050,"relativeEntities":1051,"slug":1052,"properties":1053,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"ca5ba4c9-da50-4619-ba1b-2655ff74b73f","2024-09-19T20:30:25.809+00:00",[],"Proudman-Oceanographic-Laboratory-Department-of-Engineering-Bidston-Observatory-Birkenhead-Merseyside-L43-7RA",{"title":1054},{"EN":1055},"Proudman Oceanographic Laboratory, Department of Engineering, Bidston Observatory, Birkenhead, Merseyside, L43 7RA",{"openalex":1057,"title":1059},{"VOID":1058},"A5052703266",{"EN":1060},"J.D. Humphery",{"url":24,"publisher":1062,"properties":1087},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1063,"slug":10,"properties":1064,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1070,"manageAffiliations":1071,"indexDatabases":1072,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1065,"issn":1066,"introduce":1067,"eissn":1068,"title":1069},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[1073,1080],{"id":60,"indexDatabase":1074,"url":73,"indexYears":74,"academicFieldIds":1079,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":1075,"label":1076,"description":1077,"key":70,"publicationTags":1078,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":1081,"url":94,"indexYears":24,"academicFieldIds":1086,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":1082,"label":1083,"description":1084,"key":90,"publicationTags":1085,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":1088,"pages":1090,"issue":1092},{"VOID":1089},"31",{"VOID":1091},"107-115",{"VOID":210},31,{"total":1093,"publishYear":24,"statisticByYear":1095},{"2012":148,"2014":56,"2017":148,"2018":148,"2021":148,"2022":148},"1995-11-01",1995,[1099,1102,1105,1108,1111,1114,1117,1120,1123,1126,1129,1132,1135,1138,1141,1144,1147,1150,1153,1156,1159,1162,1165,1168,1171,1174,1177,1180,1183,1186],{"id":24,"text":1100,"url":24,"identifiers":1101},"ALLEN J. R. L. 1968. Ripples – their relations to patterns of water and sediment motion. North Holland Publishing, London.",{},{"id":24,"text":1103,"url":24,"identifiers":1104},"10.1016\u002F0278-4343(83)90012-2",{"doi":1103},{"id":24,"text":1106,"url":24,"identifiers":1107},"DICKSON R., KIDD R. B. 1986. Circulation in the Southern Rockall Trough the oceanographic setting of site 610. Reports of the Deep sea drilling programme 94, 1061–74.",{},{"id":24,"text":1109,"url":24,"identifiers":1110},"DICKSON R., GOULD W. J., GRIFFITHS C., MEDLER K. J., GMITROWICZ E. M. 1986. Seasonality in currents of the Rockall Channel. Proceedings of the Royal Society of Edinburgh 88B, 103–25.",{},{"id":24,"text":1112,"url":24,"identifiers":1113},"ELLETT D. J., ROBERTS D. G. 1973. The overflow of Norwegian Sea Deep Water across the Wyville-Thomson Ridge. Deep-Sea Research 20, 819–35.",{},{"id":24,"text":1115,"url":24,"identifiers":1116},"10.1016\u002F0037-0738(93)90127-Q",{"doi":1115},{"id":24,"text":1118,"url":24,"identifiers":1119},"FRITZ W. J., MOORE J. N. 1988. Basics of Physical stratigraphy and sedimentology. J. Wiley and Sons.",{},{"id":24,"text":1121,"url":24,"identifiers":1122},"GAGE J. D., PEARSON M., CLARK A. M., PATERSON G. L. T., TYLER P. A. 1983. Echinoderms of the Rockall Trough and adjacent areas, Part I: Asteroidea and Ophiuriodea. Bulletin of the British Museum, Natural History (Zoology) 45, 263–308.",{},{"id":24,"text":1124,"url":24,"identifiers":1125},"GAGE J. D., BILLET D. S. M., JENSEN M., TYLER P. A. 1985. Echinoderms of the Rockall Trough and adjacent areas, Part II: Echinoidea and Holothurioidea. Bulletin of the British Museum, Natural History (Zoology) 48, 173–213.",{},{"id":24,"text":1127,"url":24,"identifiers":1128},"10.1016\u002F0025-3227(91)90045-6",{"doi":1127},{"id":24,"text":1130,"url":24,"identifiers":1131},"10.1016\u002F0198-0149(82)90025-5",{"doi":1130},{"id":24,"text":1133,"url":24,"identifiers":1134},"10.1126\u002Fscience.152.3721.502",{"doi":1133},{"id":24,"text":1136,"url":24,"identifiers":1137},"10.1016\u002F0967-0637(93)90127-O",{"doi":1136},{"id":24,"text":1139,"url":24,"identifiers":1140},"HOLLISTER C. D., HEEZEN B. C. 1972. Geological effects of bottom currents, Western North Atlantic. In , Gordon A. L. (Ed.), Studies in Physical Oceanography 2, 37–66. Gordon and Breach, New York.",{},{"id":24,"text":1142,"url":24,"identifiers":1143},"10.1038\u002F309220a0",{"doi":1142},{"id":24,"text":1145,"url":24,"identifiers":1146},"10.1016\u002F0025-3227(91)90055-9",{"doi":1145},{"id":24,"text":1148,"url":24,"identifiers":1149},"10.1016\u002F0025-3227(91)90044-5",{"doi":1148},{"id":24,"text":1151,"url":24,"identifiers":1152},"10.1016\u002F0037-0738(94)00121-A",{"doi":1151},{"id":24,"text":1154,"url":24,"identifiers":1155},"10.1029\u002F94PA01440",{"doi":1154},{"id":24,"text":1157,"url":24,"identifiers":1158},"HUTHNANCE J. M. 1986. Rockall slope current and shelf edge processes. Proceedings of the Royal Society of Edinburgh 88B, 83–101.",{},{"id":24,"text":1160,"url":24,"identifiers":1161},"10.1016\u002F0025-3227(86)90106-4",{"doi":1160},{"id":24,"text":1163,"url":24,"identifiers":1164},"LONSDALE P., HOLLISTER C. D. 1979. A near-bottom traverse of the Rockall Trough: Hydrographic and Geologic inferences. Oceanologica Acta 2, 91–105.",{},{"id":24,"text":1166,"url":24,"identifiers":1167},"10.1016\u002F0079-6611(92)90006-L",{"doi":1166},{"id":24,"text":1169,"url":24,"identifiers":1170},"McCAVE I. N., TUCHOLKE B. E. 1986. Deep current controlled sedimentation in the Western North Atlantic. In , Vogt P. R., Tucholke B. E. (eds). Western North Atlantic-Region. Geology of North America M, 451–68.Geological Society of America.",{},{"id":24,"text":1172,"url":24,"identifiers":1173},"10.1016\u002F0037-0738(93)90123-M",{"doi":1172},{"id":24,"text":1175,"url":24,"identifiers":1176},"PATERSON G. L. J., TYLER P. A., GAGE J. D. 1982. Taxonomy and Zoogeography of the genus Ophiocten in the North Atlantic Ocean. Bulletin of the British Museum of Natural History (Zoology) 43, 109–28.",{},{"id":24,"text":1178,"url":24,"identifiers":1179},"PICKERING K. T., HISCOTT R. N., HEIN F. J. 1989. Deep marine environments: clastic sedimentation and tectonics. Unwin Hyman, London.",{},{"id":24,"text":1181,"url":24,"identifiers":1182},"10.1144\u002Fgsjgs.151.2.0235",{"doi":1181},{"id":24,"text":1184,"url":24,"identifiers":1185},"STOW D. A. V., HOLBROOK J. A. 1984. North Atlantic contourites: an overview. In , Stow D. A. V., Piper D. J. W. (eds.), Fine-grained sediments deep-water processes and facies. Geological Society, London, Special Publication 15, 245–56.",{},{"id":24,"text":1187,"url":24,"identifiers":1188},"10.1016\u002F0012-8252(79)90002-3",{"doi":1187},{"id":1190,"createTime":1191,"updateTime":1191,"relativeEntities":1192,"slug":1193,"properties":1194,"entityType":119,"verifyStatus":23,"verifyTime":1191,"verifyNote":1206,"syncStatus":23,"languages":1207,"translateLanguages":24,"viewCount":25,"primaryUrl":1208,"fullTextUrl":24,"authors":1209,"publicationType":177,"publisherRelationship":1237,"citationCount":1269,"citationInfo":1270,"publishDate":1272,"publishYear":1273,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1274,"isForceReanalyzing":399},"4c4145e0-d942-4ae9-85ea-a5ce3f8dcfd7","2024-09-19T20:30:10.384+00:00",[],"A-local-deep-water-sediment-failure-on-the-NW-slope-of-the-UK",{"mag":1195,"keywords":1197,"openalex":1198,"abstract":1200,"title":1202,"doi":1204},{"VOID":1196},"2069656905",{},{"VOID":1199},"W2069656905",{"EN":1201},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>An example is described, from seismic evidence, of a local deep-water sediment failure on the slope to the west of the Isle of Lewis, an area which otherwise appears to be generally stable. The feature is about 4 km long in the downslope direction and lies above an escarpment at an approximate water depth of 1100 m. The loss of layering on the reflection profile, and the existence of infilled depressions, suggests that excess pore water pressures have been generated and subsequently dissipated. It is conjectured that the failure has been triggered by an earthquake, or possibly by internal wave action. The sediment body is thought to have failed by liquefaction acting retrogressively upslope.\u003C\u002Fjats:p>",{"EN":1203},"A local deep-water sediment failure on the NW slope of the UK",{"VOID":1205},"10.1144\u002Fsjg27020107","Author affiliation is blank",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg27020107",[1210,1229],{"id":1211,"sortIndex":25,"researcher":24,"roles":1212,"affiliations":1213,"properties":1224},"452af711-5689-40fe-9dc8-aff11433ba75",[],[1214],{"id":1215,"sortIndex":25,"affiliation":1216,"properties":24},"e4083d1d-441b-46f0-8ebd-1587a2a63eaf",{"id":1217,"createTime":1218,"updateTime":1218,"relativeEntities":1219,"slug":1220,"properties":1221,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"ec30ba2a-5b1e-44ae-b24b-afe708ffc018","2024-09-19T20:30:10.401+00:00",[],"Energy-Simulation-Research-Unit-University-of-Strathclyde-Glasgow",{"title":1222},{"EN":1223},"Energy Simulation Research Unit, University of Strathclyde, Glasgow",{"openalex":1225,"title":1227},{"VOID":1226},"A5087085517",{"EN":1228},"P. Strachan",{"id":1230,"sortIndex":148,"researcher":24,"roles":1231,"affiliations":1232,"properties":1233},"5bc7b4f1-a24c-43cf-bc2e-521465476421",[],[],{"openalex":1234,"orcid":1235,"title":1236},{"VOID":649},{"VOID":651},{"EN":653},{"url":24,"publisher":1238,"properties":1263},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1239,"slug":10,"properties":1240,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1246,"manageAffiliations":1247,"indexDatabases":1248,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1241,"issn":1242,"introduce":1243,"eissn":1244,"title":1245},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[1249,1256],{"id":60,"indexDatabase":1250,"url":73,"indexYears":74,"academicFieldIds":1255,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":1251,"label":1252,"description":1253,"key":70,"publicationTags":1254,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":1257,"url":94,"indexYears":24,"academicFieldIds":1262,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":1258,"label":1259,"description":1260,"key":90,"publicationTags":1261,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":1264,"pages":1266,"issue":1268},{"VOID":1265},"27",{"VOID":1267},"107-111",{"VOID":210},12,{"total":1269,"publishYear":24,"statisticByYear":1271},{"2012":148,"2014":148,"2016":148,"2017":148,"2020":148},"1991-12-01",1991,[1275,1278,1281,1284,1286,1289,1292,1295,1298,1301,1304,1307,1309,1311,1314,1317,1319],{"id":24,"text":1276,"url":24,"identifiers":1277},"10.1007\u002F978-94-009-7046-5_30",{"doi":1276},{"id":24,"text":1279,"url":24,"identifiers":1280},"10.1016\u002F0025-3227(90)90049-P",{"doi":1279},{"id":24,"text":1282,"url":24,"identifiers":1283},"EVANS D. 1987. Geikie 58°N–10°W Quaternary. 1:250 000 Map Series British Geological Survey .",{},{"id":24,"text":629,"url":24,"identifiers":1285},{"doi":629},{"id":24,"text":1287,"url":24,"identifiers":1288},"EVANS D. STRACHAN P. A. 1987. Geikie 58°N–10°W Seabed Sediments. 1:250 000 Map Series British Geological Survey .",{},{"id":24,"text":1290,"url":24,"identifiers":1291},"10.1130\u002F0091-7613(1982)10\u003C542:ESFOAS>2.0.CO;2",{"doi":1290},{"id":24,"text":1293,"url":24,"identifiers":1294},"10.1007\u002F978-94-009-2311-9",{"doi":1293},{"id":24,"text":1296,"url":24,"identifiers":1297},"10.1680\u002Fgeot.1970.20.1.75",{"doi":1296},{"id":24,"text":1299,"url":24,"identifiers":1300},"HOVLAND M., JUDD A. G. 1988. Seabed pockmarks and seepages. Graham and Trotman Ltd.",{},{"id":24,"text":1302,"url":24,"identifiers":1303},"10.1144\u002Fsjg19030287",{"doi":1302},{"id":24,"text":1305,"url":24,"identifiers":1306},"JONES E. J. W., PERRY R. G., WILD J. L. 1986. Geology of the Hebridean margin of the Rockall Trough. Proc. R. Soc. Edinb. 88b, 27–51.",{},{"id":24,"text":1160,"url":24,"identifiers":1308},{"doi":1160},{"id":24,"text":775,"url":24,"identifiers":1310},{"doi":775},{"id":24,"text":1312,"url":24,"identifiers":1313},"MORGENSTERN N. R. 1967. Submarine slumping and the initiation of turbidity currents. In , Richards A., Marine Geotechnique, 189–220, Univ. Illinois Press, Urbana.",{},{"id":24,"text":1315,"url":24,"identifiers":1316},"10.1007\u002F978-1-4613-3362-3_3",{"doi":1315},{"id":24,"text":793,"url":24,"identifiers":1318},{"doi":793},{"id":24,"text":1320,"url":24,"identifiers":1321},"SEED H. B. 1979. Soil liquefaction and cyclic mobility evaluation for level ground during earthquakes. Am. Soc. Civ. Eng. 105, (GT2), 201–55.",{},{"id":1323,"createTime":1324,"updateTime":1324,"relativeEntities":1325,"slug":1326,"properties":1327,"entityType":119,"verifyStatus":120,"verifyTime":1324,"verifyNote":121,"syncStatus":23,"languages":1339,"translateLanguages":24,"viewCount":25,"primaryUrl":1340,"fullTextUrl":24,"authors":1341,"publicationType":177,"publisherRelationship":1362,"citationCount":1395,"citationInfo":1396,"publishDate":1407,"publishYear":1408,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1409,"isForceReanalyzing":399},"23dd6bdd-153f-4c00-a8c2-2977e47579d7","2024-11-30T19:24:34.540+00:00",[],"Magmatism-of-the-British-Tertiary-Volcanic-Province",{"mag":1328,"keywords":1330,"openalex":1331,"abstract":1333,"title":1335,"doi":1337},{"VOID":1329},"1967156352",{},{"VOID":1332},"W1967156352",{"EN":1334},"\u003Cjats:title>Synopsis\u003C\u002Fjats:title>\n          \u003Cjats:p>This review concentrates on those aspects of research into the magmatism of the British Tertiary Volcanic Province (BTVP) which have seen rapid accumulation of data and changes of views during the last few years. There seems to be general agreement at present amongst those who have made detailed geochemical studies of the problem that the pervasive hydrothermal metamorphism which affects most BTVP igneous rocks has not caused significant changes in the compositions (other than hydrogen and oxygen isotopes) of samples collected away from the immediate vicinities of the major passageways for hydrothermal fluids. Wide ranges of silica saturation characterize the basic members of both the major traditional BTVP magma types—Plateau and Non-Porphyritic Central (NPC). It is only the evolved members of these suites, the ne-normative Plateau-type hawaiites and the Q-normative NPC tholeiitic andesites, which show clearly the long-emphasized contrast between alkalic and tholeiitic compositions. Prior to their final uprise and eruption or emplacement, the Plateau-type magmas appear to have equilibrated near the base of the continental crust, whereas the NPC magmas evolved at upper-crustal depths. The NPC basalts (as traditionally defined) seem to be polygenetic in terms of mantle-derived magma types. Most of them are related to the MORB(Mid Ocean Ridge Basalt)-like Preshal Mhor basalts of Skye and Mull but some appear to be batches of Plateau-type magma which equilibrated in the upper crust. The Rio Grande Rift, southwestern U.S.A., provides a present-day analogue to the Palaeocene magmatic plumbing envisaged beneath the BTVP.\u003C\u002Fjats:p>\n          \u003Cjats:p>The mantle-derived basic magmas upwelling beneath the BTVP were affected by fractional crystallisation and sialic contamination to varying extents as they rose through the continental crust. The earlier magma batches mostly interacted only with granulite-facies Lewisian gneisses, from which they appear to have melted selectively the most-fusible minor acid members. In addition, there is little doubt that Pb equilibrated selectively, in a vapour or non-silicate liquid phase, between the magmas and Archean sial, whilst Sr- and Nd-isotope ratios in the BTVP igneous rocks may also be in part the products of selective magma-crust interactions. If those BTVP basic rocks which contain negligible components of sialic contaminant are considered, it is apparent that there are consistent differences in various incompatible-element ratios between the Plateau-type basalts of Skye and Mull, the two areas studied in most detail at present. All of the BTVP Plateau-type basalts are exceptionally depleted in the strongly-incompatible elements, relative to worldwide examples of basalts with similar major-element compositions. This feature is consistent with genesis from a volume of upper mantle which had previously lost a very small fraction of strongly-alkalic melt. The Permian lamprophyres of the region are tentatively identified as samples of this postulated pre-Tertiary alkalic magma. A case is also made for considering the Caledonian Iapetus Suture as the tectonic feature along which most of the BTVP igneous centres are distributed. Seen from this point of view, the origins of BTVP magmatism are to be found in upper-mantle convection during and after the subduction which closed Iapetus—subsequently re-activated by the regional tension and Palaeocene mantle convection associated with the opening of the North Atlantic. At the climax of BTVP magmatism, when the bulk of the dyke swarms and the plutons of the central complexes were emplaced, a final increment of the progressive partial fusion of the upper mantle beneath the region gave rise to the MORB-like Preshal Mhor-type magmas.\u003C\u002Fjats:p>\n          \u003Cjats:p>Although it is apparent from their Sr-, Nd- and Pb-isotope ratios that most of the BTVP acid magmas contained appreciable fractions from sialic sources, there are few instances where mantle-derived magma does not appear to have been the dominant ingredient in the hybrid liquids which evolved—by fractional crystallisation—to acid residua. Nevertheless, when the sequence of granite emplacement within individual BTVP intrusive centres is considered, it is apparent that the evolution of each acid magma batch was a complex and variable process, involving combinations of such mechanisms as fractional crystallisation, fusion of both sialic crust and earlier BTVP acid rocks, and mixing of magmas at various states of evolution.\u003C\u002Fjats:p>",{"EN":1336},"Magmatism of the British Tertiary Volcanic Province",{"VOID":1338},"10.1144\u002Fsjg18010049",[123],"https:\u002F\u002Fwww.lyellcollection.org\u002Fdoi\u002F10.1144\u002Fsjg18010049",[1342],{"id":1343,"sortIndex":25,"researcher":24,"roles":1344,"affiliations":1345,"properties":1357},"30bd860e-848d-4d93-83b5-413e8e6f3eef",[],[1346],{"id":1347,"sortIndex":25,"affiliation":1348,"properties":24},"4832004b-cd21-4a57-9ea4-b7b619b9c7c5",{"id":1349,"createTime":1350,"updateTime":1351,"relativeEntities":1352,"slug":1353,"properties":1354,"entityType":45,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"9bd7e87c-0a81-4dd3-9bf3-0bf80d798382","2024-11-30T19:24:34.562+00:00","2025-01-31T18:49:13.126+00:00",[],"Department-of-Geology-Imperial-College-of-Science-and-Technology-London-SW7-2BP",{"title":1355},{"EN":1356},"Department of Geology, Imperial College of Science and Technology, London SW7 2BP",{"openalex":1358,"title":1360},{"VOID":1359},"A5024868222",{"EN":1361},"R. N. Thompson",{"url":24,"publisher":1363,"properties":1388},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1364,"slug":10,"properties":1365,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1371,"manageAffiliations":1372,"indexDatabases":1373,"url":97,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1366,"issn":1367,"introduce":1368,"eissn":1369,"title":1370},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[1374,1381],{"id":60,"indexDatabase":1375,"url":73,"indexYears":74,"academicFieldIds":1380,"indexDatabaseRanking":77},{"id":62,"createTime":63,"updateTime":64,"relativeEntities":1376,"label":1377,"description":1378,"key":70,"publicationTags":1379,"standard":24},[],{"EN":67,"VI":67},{"EN":67,"VI":69},[72],[76],{"id":79,"indexDatabase":1382,"url":94,"indexYears":24,"academicFieldIds":1387,"indexDatabaseRanking":24},{"id":81,"createTime":82,"updateTime":83,"relativeEntities":1383,"label":1384,"description":1385,"key":90,"publicationTags":1386,"standard":24},[],{"EN":86,"VI":86},{"VI":88,"EN":89},[92,93],[96],{"volume":1389,"pages":1391,"issue":1393},{"VOID":1390},"18",{"VOID":1392},"49-107",{"VOID":1394},"1",661,{"total":1395,"publishYear":24,"statisticByYear":1397},{"2012":211,"2013":1398,"2014":888,"2015":723,"2016":1399,"2017":1400,"2018":1401,"2019":1402,"2020":1403,"2021":1401,"2022":1404,"2023":1405,"2024":1406},13,28,32,25,33,21,6,24,10,"1982-02-01",1982,[1410,1413,1416,1419,1422,1425,1428,1431,1434,1437,1440,1443,1446,1449,1452,1455,1458,1461,1464,1467,1470,1473,1476,1479,1482,1485,1488,1491,1494,1497,1500,1503,1506,1509,1512,1515,1518,1521,1524,1527,1530,1533,1536,1539,1542,1545,1548,1551,1554,1557,1560,1563,1566,1569,1572,1575,1578,1581,1584,1587,1590,1593,1596,1599,1602,1605,1608,1611,1614,1617,1620,1623,1626,1630,1633,1636,1639,1642,1645,1648,1651,1654,1657,1660,1663,1666,1669,1672,1676,1679,1682,1686,1689,1692,1695,1698,1701,1704,1707,1711,1714,1717,1720,1723,1726,1729,1732,1735,1738,1741,1744,1747,1750,1753,1757,1760,1763,1766,1770,1773,1776,1779,1782,1785,1788,1791,1794,1797,1800,1803,1806,1809,1812,1815,1818,1821,1824,1827,1830,1833,1836,1839,1842,1845,1848,1852,1855,1858,1861,1864,1867,1870,1873,1876,1879,1882,1885,1888,1891,1894,1897,1900,1903],{"id":24,"text":1411,"url":24,"identifiers":1412},"AOKI K., KUDO A. M. 1976. Major-element variations of late Cenozoic Basalts of New Mexico. New Mexico Geol. Soc. Spec. Publ. 5, 82–8.",{},{"id":24,"text":1414,"url":24,"identifiers":1415},"ANDERSON F. W., DUNHAM K. C. 1966. The geology of northern Skye, Mem. Geol. Surv. G.B.",{},{"id":24,"text":1417,"url":24,"identifiers":1418},"BAILEY E. B., CLOUGH C. T., WRIGHT W. B., RICHEY J. E., WILSON G. V. 1924. Tertiary and post-Tertiary geology of Mull, Loch Aline and Oban. Mem. Geol. Surv. G.B.",{},{"id":24,"text":1420,"url":24,"identifiers":1421},"BALDRIDGE W. S. 1979. Petrology and petrogenesis of Plio-Pleistocene basaltic rocks from the Central Rio Grande Rift, New Mexico and their relation to rift structure. In , Riecker R. E. (ed.) Rio Grande Rift: tectonics and magmatism, 323–53, Am. Geophys. U.",{},{"id":24,"text":1423,"url":24,"identifiers":1424},"10.1016\u002F0012-821X(80)90213-7",{"doi":1423},{"id":24,"text":1426,"url":24,"identifiers":1427},"10.1144\u002Fgsjgs.133.5.0481",{"doi":1426},{"id":24,"text":1429,"url":24,"identifiers":1430},"10.1016\u002F0012-821X(74)90090-9",{"doi":1429},{"id":24,"text":1432,"url":24,"identifiers":1433},"10.1007\u002FBF00403427",{"doi":1432},{"id":24,"text":1435,"url":24,"identifiers":1436},"10.1017\u002FS0080456800023632",{"doi":1435},{"id":24,"text":1438,"url":24,"identifiers":1439},"10.1016\u002FS0016-7878(76)80001-6",{"doi":1438},{"id":24,"text":1441,"url":24,"identifiers":1442},"10.1144\u002Fgsjgs.121.1.0031",{"doi":1441},{"id":24,"text":1444,"url":24,"identifiers":1445},"10.1038\u002Fphysci242114a0",{"doi":1444},{"id":24,"text":1447,"url":24,"identifiers":1448},"BOWEN N. L. 1928. The evolution of the igneous rocks, Princeton University Press.",{},{"id":24,"text":1450,"url":24,"identifiers":1451},"10.1016\u002F0079-1946(75)90055-5",{"doi":1450},{"id":24,"text":1453,"url":24,"identifiers":1454},"10.1126\u002Fscience.193.4258.1086",{"doi":1453},{"id":24,"text":1456,"url":24,"identifiers":1457},"10.1180\u002Fminmag.1963.033.262.02",{"doi":1456},{"id":24,"text":1459,"url":24,"identifiers":1460},"10.1144\u002Fgsjgs.119.1.0095",{"doi":1459},{"id":24,"text":1462,"url":24,"identifiers":1463},"10.1126\u002Fscience.202.4369.743",{"doi":1462},{"id":24,"text":1465,"url":24,"identifiers":1466},"10.1144\u002Fsjg15040333",{"doi":1465},{"id":24,"text":1468,"url":24,"identifiers":1469},"CLAGUE D. A., FREY F. A. 1981. Petrology and trace-element geochemistry of the Honolulu Volcanic Series, Oahu : implications for the oceanic mantle below Hawaii. J. Petrol, (in press).",{},{"id":24,"text":1471,"url":24,"identifiers":1472},"CLARKE E., BECKINSALE R. D., SKELHORN R. R., THORPE R. S., WALSH J. N. 1980. A basic-to-acid fractional crystallisation sequence from Mull. Mineral. Soc. Bull. 47–8, 2.",{},{"id":24,"text":1474,"url":24,"identifiers":1475},"10.1038\u002F283149a0",{"doi":1474},{"id":24,"text":1477,"url":24,"identifiers":1478},"10.1016\u002F0012-821X(79)90048-7",{"doi":1477},{"id":24,"text":1480,"url":24,"identifiers":1481},"10.1016\u002F0012-821X(78)90116-4",{"doi":1480},{"id":24,"text":1483,"url":24,"identifiers":1484},"10.1016\u002F0016-7037(78)90003-0",{"doi":1483},{"id":24,"text":1486,"url":24,"identifiers":1487},"10.1093\u002Fpetrology\u002F22.2.155",{"doi":1486},{"id":24,"text":1489,"url":24,"identifiers":1490},"10.1007\u002FBF00373689",{"doi":1489},{"id":24,"text":1492,"url":24,"identifiers":1493},"10.1016\u002F0012-821X(80)90257-5",{"doi":1492},{"id":24,"text":1495,"url":24,"identifiers":1496},"10.1093\u002Fpetrology\u002F18.4.595",{"doi":1495},{"id":24,"text":1498,"url":24,"identifiers":1499},"10.1093\u002Fpetrology\u002F7.3.414",{"doi":1498},{"id":24,"text":1501,"url":24,"identifiers":1502},"10.1016\u002F0009-2541(72)90055-1",{"doi":1501},{"id":24,"text":1504,"url":24,"identifiers":1505},"10.1144\u002Fsjg16020199",{"doi":1504},{"id":24,"text":1507,"url":24,"identifiers":1508},"10.1038\u002F286017a0",{"doi":1507},{"id":24,"text":1510,"url":24,"identifiers":1511},"DURANT G. P. 1978. The geochemistry of the Tertiary Islay and Jura dyke swarms. J. Geol. Soc 135, 463.",{},{"id":24,"text":1513,"url":24,"identifiers":1514},"EATON G. P. 1979. A plate tectonic model for Late Cenozoic crustal spreading in the western United States. In , Riecker R. E. (ed.) Rio Grande Rift: tectonics and magmatism, 7–32, Am. Geophys. U.",{},{"id":24,"text":1516,"url":24,"identifiers":1517},"EMELEUS C. H., DUNHAM A. C., THOMPSON R. N. 1971. Iron-rich pigeonites from acid rocks in the Tertiary Igneous Province of Scotland. Am. Mineral. 56, 940–51.",{},{"id":24,"text":1519,"url":24,"identifiers":1520},"10.1093\u002Fpetrology\u002F16.1.488",{"doi":1519},{"id":24,"text":1522,"url":24,"identifiers":1523},"FLANAGAN F. J. 1978. Descriptions and analyses of eight new USGS rock standards. U.S. Geol. Surv. Prof. Paper 840, 1–192.",{},{"id":24,"text":1525,"url":24,"identifiers":1526},"FORD C. E., MACDONALD R. 1978. Melting relations of a Midland Valley alkali basalt. NERC Pub. D11, 196–7.",{},{"id":24,"text":1528,"url":24,"identifiers":1529},"10.1016\u002F0012-821X(76)90178-3",{"doi":1528},{"id":24,"text":1531,"url":24,"identifiers":1532},"10.2475\u002Fajs.277.2.136",{"doi":1531},{"id":24,"text":1534,"url":24,"identifiers":1535},"10.1093\u002Fpetrology\u002F19.3.463",{"doi":1534},{"id":24,"text":1537,"url":24,"identifiers":1538},"10.1007\u002FBF00375190",{"doi":1537},{"id":24,"text":1540,"url":24,"identifiers":1541},"10.1016\u002F0377-0273(79)90021-0",{"doi":1540},{"id":24,"text":1543,"url":24,"identifiers":1544},"GAMBLE J. A., OLD R. A., PRESTON J. 1976. Subsurface exploration in the Tertiary central complex of gabbro and granophyre at Slieve Gullion, Co. Armagh, Northern Ireland. Rep. Inst. Geol. Sci. No. 76\u002F8.",{},{"id":24,"text":1546,"url":24,"identifiers":1547},"GASS I. G., THORPE R. S. 1976. Igneous case study: the Tertiary igneous rocks of Skye, NW Scotland. In , Aprahamian F. (ed.), Science: a third level course. Earth science topics and methods, Open University Press.",{},{"id":24,"text":1549,"url":24,"identifiers":1550},"10.1144\u002Fsjg14010001",{"doi":1549},{"id":24,"text":1552,"url":24,"identifiers":1553},"10.1144\u002Fgsjgs.117.1.0233",{"doi":1552},{"id":24,"text":1555,"url":24,"identifiers":1556},"10.1144\u002Fsjg10010071",{"doi":1555},{"id":24,"text":1558,"url":24,"identifiers":1559},"HALSALL T. J. 1978. The emplacement of the Tertiary dykes of the Kildonan shore, south Arran. J. Geol. Soc. 135, 462.",{},{"id":24,"text":1561,"url":24,"identifiers":1562},"10.1038\u002F277025a0",{"doi":1561},{"id":24,"text":1564,"url":24,"identifiers":1565},"HARKER A. 1904. The Tertiary igneous rocks of Skye. Mem. Geol. Surv. G. B.",{},{"id":24,"text":1567,"url":24,"identifiers":1568},"HARRISON R. K., JEANS C. V., MERRIMAN R. J. 1979. Mesozoic igneous rocks, hydrothermal mineralisation and volcanogenic sediments in Britain and adjacent areas. Bull. Geol. Surv. G.B. 70, 57–69.",{},{"id":24,"text":1570,"url":24,"identifiers":1571},"10.1038\u002F276381a0",{"doi":1570},{"id":24,"text":1573,"url":24,"identifiers":1574},"10.1144\u002Fsjg12040325",{"doi":1573},{"id":24,"text":1576,"url":24,"identifiers":1577},"10.1007\u002FBF00371073",{"doi":1576},{"id":24,"text":1579,"url":24,"identifiers":1580},"10.1017\u002FS0016756800037754",{"doi":1579},{"id":24,"text":1582,"url":24,"identifiers":1583},"10.1180\u002Fminmag.1929.022.124.03",{"doi":1582},{"id":24,"text":1585,"url":24,"identifiers":1586},"10.1016\u002F0009-2541(78)90070-0",{"doi":1585},{"id":24,"text":1588,"url":24,"identifiers":1589},"10.1017\u002FS0016756800053024",{"doi":1588},{"id":24,"text":1591,"url":24,"identifiers":1592},"JOHNSON G. A. L. 1978. European plate movement during the Carboniferous. In , Tarling D. H. (ed.), Evolution of the Earth's crust, 343–60, Academic Press.",{},{"id":24,"text":1594,"url":24,"identifiers":1595},"KENNEDY W. Q. 1930. The parent magma of the British Tertiary Province. Geol. Surv. G.B. Summ. Prog. II, 61–73.",{},{"id":24,"text":1597,"url":24,"identifiers":1598},"KING P. 1977. The secondary minerals of the Tertiary lavas of northern and central Skye—zeolite zonation patterns their origin and formation. Univ. Aberdeen Ph.D. thesis (unpubl.).",{},{"id":24,"text":1600,"url":24,"identifiers":1601},"10.1016\u002F0012-821X(77)90194-7",{"doi":1600},{"id":24,"text":1603,"url":24,"identifiers":1604},"Le BAS M. J. 1967. On the origin of the Tertiary granophyres of the Carlingford Complex, Ireland. Proc. R. Ir. Acad. 65B, 325–38.",{},{"id":24,"text":1606,"url":24,"identifiers":1607},"10.1038\u002F281365a0",{"doi":1606},{"id":24,"text":1609,"url":24,"identifiers":1610},"10.1130\u002F0016-7606(1976)87\u003C1777:POMBSR>2.0.CO;2",{"doi":1609},{"id":24,"text":1612,"url":24,"identifiers":1613},"10.1130\u002F0091-7613(1979)7\u003C384:IAAHOI>2.0.CO;2",{"doi":1612},{"id":24,"text":1615,"url":24,"identifiers":1616},"LONG L. E., LAMBERT R. St. J. 1963. Rb-Sr ages from the Moine Series. In , Johnson M. R. W., Stewart F. H. (eds.), The British Caledonides, 217–47, Oliver and Boyd.",{},{"id":24,"text":1618,"url":24,"identifiers":1619},"LYLE P. 1980. A petrological and geochemical study of the Tertiary basaltic rocks of Northeast Ireland. J. Earth Sci. R. Dubl. Soc. 2, 137–52.",{},{"id":24,"text":1621,"url":24,"identifiers":1622},"10.1144\u002Fsjg11040333",{"doi":1621},{"id":24,"text":1624,"url":24,"identifiers":1625},"10.1144\u002Fsjg11040269",{"doi":1624},{"id":24,"text":1627,"url":24,"identifiers":1628},"MACDONALD R. 1980. Trace element evidence for mantle heterogeneity beneath the Scottish Midland Valley in the Carboniferous and Permian. Philos. Trans. R. Soc. Lond. A297, 245–57.",{"doi":1629},"10.1098\u002Frsta.1980.0213",{"id":24,"text":1631,"url":24,"identifiers":1632},"MASON B. 1979. Data of geochemistry. Chapter B. Cosmochemistry. Part 1. Meteorites. Prof. Pap. U.S. Geol. Surv. 440-B-1, 1–132.",{},{"id":24,"text":1634,"url":24,"identifiers":1635},"MATTEY D. P. 1980. The petrology of high-calcium low-alkali tholeiite dykes from the Isle of Skye regional swarm. Univ. London Ph.D. thesis (unpubl.).",{},{"id":24,"text":1637,"url":24,"identifiers":1638},"10.1180\u002Fminmag.1977.041.318.16",{"doi":1637},{"id":24,"text":1640,"url":24,"identifiers":1641},"MEIGHAN I. G. 1979. The acid rocks of the British Tertiary Province. Bull. Geol. Surv. G.B. 70, 10–22.",{},{"id":24,"text":1643,"url":24,"identifiers":1644},"10.1016\u002F0012-821X(80)90048-5",{"doi":1643},{"id":24,"text":1646,"url":24,"identifiers":1647},"10.1016\u002F0012-821X(76)90054-6",{"doi":1646},{"id":24,"text":1649,"url":24,"identifiers":1650},"10.1017\u002FS0016756800041273",{"doi":1649},{"id":24,"text":1652,"url":24,"identifiers":1653},"10.1093\u002Fpetrology\u002F6.1.37",{"doi":1652},{"id":24,"text":1655,"url":24,"identifiers":1656},"10.1144\u002Fsjg03030389",{"doi":1655},{"id":24,"text":1658,"url":24,"identifiers":1659},"10.1093\u002Fpetrology\u002F21.2.295",{"doi":1658},{"id":24,"text":1661,"url":24,"identifiers":1662},"10.1016\u002FS0012-821X(68)80044-5",{"doi":1661},{"id":24,"text":1664,"url":24,"identifiers":1665},"MORRISON M. A. 1977. Interactions between water and Palaeocene basalt, Mull, NW Scotland. Abstr. IASPEI\u002FIAVCEI meeting, Durham, 250.",{},{"id":24,"text":1667,"url":24,"identifiers":1668},"10.1016\u002F0012-821X(78)90029-8",{"doi":1667},{"id":24,"text":1670,"url":24,"identifiers":1671},"MORRISON M. A. 1980. Igneous and metamorphic geochemistry of Mull lavas. Univ. London Ph.D. thesis (unpubl.).",{},{"id":24,"text":1673,"url":24,"identifiers":1674},"MORRISON M. A., THOMPSON R. N., GIBSON I. L., MARRINER G. F. 1980. Lateral chemical heterogeneity in the Palaeocene upper mantle beneath the Scottish Hebrides. Philos. Trans. R. Soc. Lond. A297, 229–44.",{"doi":1675},"10.1098\u002Frsta.1980.0212",{"id":24,"text":1677,"url":24,"identifiers":1678},"MURATA K. J., RICHTER D. H. 1966. Chemistry of the lavas. 1959–60 eruption of Kilauea volcano, Hawaii. Prof. Paper U.S. Geol. Surv. 537-A, 1–26.",{},{"id":24,"text":1680,"url":24,"identifiers":1681},"10.1016\u002F0016-7037(74)90149-5",{"doi":1680},{"id":24,"text":1683,"url":24,"identifiers":1684},"O'HARA M. J. 1980. Nonlinear nature of the unavoidable long-lived isotopic, trace and major element contamination of a developing magma chamber. Philos. Trans. R. Soc. Lond. A297, 215–27.",{"doi":1685},"10.1098\u002Frsta.1980.0211",{"id":24,"text":1687,"url":24,"identifiers":1688},"10.1144\u002Fgsjgs.134.2.0255",{"doi":1687},{"id":24,"text":1690,"url":24,"identifiers":1691},"PANKHURST R. J., BECKINSALE R. D. 1979. Rare-earth evidence for the petrogenesis of Tertiary Mull volcanics. J. Geol. Soc. 136, 327.",{},{"id":24,"text":1693,"url":24,"identifiers":1694},"10.1016\u002F0012-821X(78)90109-7",{"doi":1693},{"id":24,"text":1696,"url":24,"identifiers":1697},"10.1038\u002F283559a0",{"doi":1696},{"id":24,"text":1699,"url":24,"identifiers":1700},"10.1144\u002Fgsjgs.132.6.0579",{"doi":1699},{"id":24,"text":1702,"url":24,"identifiers":1703},"10.1002\u002Fgj.3350110202",{"doi":1702},{"id":24,"text":1705,"url":24,"identifiers":1706},"RIDLEY W. I. 1973. The petrology of volcanic rocks from the Small Isles of Inverness-shire. Rep. Inst. Geol. Sci. No. 73\u002F10.",{},{"id":24,"text":1708,"url":24,"identifiers":1709},"RIECKER R. E. (ed.) 1979. Rio Grande Rift: tectonics and magmatism Am. Geophys. U.",{"doi":1710},"10.1029\u002FSP014",{"id":24,"text":1712,"url":24,"identifiers":1713},"RINEHART E. J., SANFORD A. R., WARD R. M. 1979. Geographic extent and shape of an extensive magma body at midcrustal depths in the Rio Grande Rift near Socorro, New Mexico. In , Riecker R. E. (ed.), Rio Grande Rift: tectonics and magmatism, 237–51, Am. Geophys. U.",{},{"id":24,"text":1715,"url":24,"identifiers":1716},"10.1017\u002FS0016756800043363",{"doi":1715},{"id":24,"text":1718,"url":24,"identifiers":1719},"10.1007\u002FBF00376145",{"doi":1718},{"id":24,"text":1721,"url":24,"identifiers":1722},"10.1144\u002Fgsjgs.137.5.0589",{"doi":1721},{"id":24,"text":1724,"url":24,"identifiers":1725},"SHERATON J. W., SKINNER A. C., TARNEY J. 1973. The geochemistry of the Scourian gneisses of the Assynt district. In , Park R. G., Tarney J. (Eds.), The Early Precambrian of Scotland and related rocks of Greenland, 13–30, Dept. of Geol., Univ. of Keele.",{},{"id":24,"text":1727,"url":24,"identifiers":1728},"10.1038\u002F289282a0",{"doi":1727},{"id":24,"text":1730,"url":24,"identifiers":1731},"10.1016\u002F0016-7037(79)90200-X",{"doi":1730},{"id":24,"text":1733,"url":24,"identifiers":1734},"10.1093\u002Fpetrology\u002F22.1.41",{"doi":1733},{"id":24,"text":1736,"url":24,"identifiers":1737},"10.1144\u002Fsjg15020161",{"doi":1736},{"id":24,"text":1739,"url":24,"identifiers":1740},"10.1017\u002FS0080456800023607",{"doi":1739},{"id":24,"text":1742,"url":24,"identifiers":1743},"10.1016\u002F0040-1951(77)90055-5",{"doi":1742},{"id":24,"text":1745,"url":24,"identifiers":1746},"10.1007\u002FBF02597146",{"doi":1745},{"id":24,"text":1748,"url":24,"identifiers":1749},"10.1038\u002F267315a0",{"doi":1748},{"id":24,"text":1751,"url":24,"identifiers":1752},"10.1007\u002FBF00375485",{"doi":1751},{"id":24,"text":1754,"url":24,"identifiers":1755},"SUN S.-S. 1980. Lead isotopic study of young volcanic rocks from mid-ocean ridges, ocean islands and island arcs. Philos. Trans. R. Soc. Lond. A297, 409–45.",{"doi":1756},"10.1098\u002Frsta.1980.0224",{"id":24,"text":1758,"url":24,"identifiers":1759},"10.1007\u002FBF00395006",{"doi":1758},{"id":24,"text":1761,"url":24,"identifiers":1762},"SUTHERLAND D. S. (ed.) 1981. Igneous rocks of the British Isles. Wiley.",{},{"id":24,"text":1764,"url":24,"identifiers":1765},"10.1017\u002FS0016756800043259",{"doi":1764},{"id":24,"text":1767,"url":24,"identifiers":1768},"TARNEY J., WOOD D. A., SAUNDERS A. D., CANN J. R., VARET J. 1980. Nature of mantle heterogeneity in the North Atlantic: evidence from deep sea drilling. Philos. Trans. R. Soc. Lond. A297, 179–202.",{"doi":1769},"10.1098\u002Frsta.1980.0209",{"id":24,"text":1771,"url":24,"identifiers":1772},"10.1093\u002Fpetrology\u002F12.3.465",{"doi":1771},{"id":24,"text":1774,"url":24,"identifiers":1775},"10.1086\u002F628526",{"doi":1774},{"id":24,"text":1777,"url":24,"identifiers":1778},"10.1144\u002Fgsjgs.138.2.0123",{"doi":1777},{"id":24,"text":1780,"url":24,"identifiers":1781},"THOMPSON R. N. 1965. The geology and petrology of the Marsco area Skye. Univ. Oxford D.Phil thesis (unpubl.).",{},{"id":24,"text":1783,"url":24,"identifiers":1784},"10.1144\u002Fgsjgs.124.1.0349",{"doi":1783},{"id":24,"text":1786,"url":24,"identifiers":1787},"10.1007\u002FBF00371750",{"doi":1786},{"id":24,"text":1789,"url":24,"identifiers":1790},"10.1007\u002FBF00457295",{"doi":1789},{"id":24,"text":1792,"url":24,"identifiers":1793},"10.1007\u002FBF01869036",{"doi":1792},{"id":24,"text":1795,"url":24,"identifiers":1796},"THOMPSON R. N. 1981a. The Tertiary Province: geochemistry and magma genesis. In , Sutherland D. S. (ed.), Igneous rocks of the British Isles, 461–77, Wiley.",{},{"id":24,"text":1798,"url":24,"identifiers":1799},"10.1180\u002Fminmag.1981.044.334.08",{"doi":1798},{"id":24,"text":1801,"url":24,"identifiers":1802},"10.1093\u002Fpetrology\u002F13.2.219",{"doi":1801},{"id":24,"text":1804,"url":24,"identifiers":1805},"10.1093\u002Fpetrology\u002F21.2.265",{"doi":1804},{"id":24,"text":1807,"url":24,"identifiers":1808},"THOMPSON R. N., MORRISON M. A., GIBSON I. L., DICKIN A. P. 1981. The Staffa Magma Type revisited . . . . and re-instated. J. Geol. Soc., in press.",{},{"id":24,"text":1810,"url":24,"identifiers":1811},"10.1016\u002F0012-821X(80)90115-6",{"doi":1810},{"id":24,"text":1813,"url":24,"identifiers":1814},"10.1180\u002Fminmag.1978.042.321.30",{"doi":1813},{"id":24,"text":1816,"url":24,"identifiers":1817},"10.1016\u002F0012-821X(77)90192-3",{"doi":1816},{"id":24,"text":1819,"url":24,"identifiers":1820},"10.1144\u002FGSL.JGS.1950.106.01-04.04",{"doi":1819},{"id":24,"text":1822,"url":24,"identifiers":1823},"10.1144\u002Ftransed.19.2.208",{"doi":1822},{"id":24,"text":1825,"url":24,"identifiers":1826},"10.1080\u002F11035896409455489",{"doi":1825},{"id":24,"text":1828,"url":24,"identifiers":1829},"10.1016\u002F0012-821X(70)90104-4",{"doi":1828},{"id":24,"text":1831,"url":24,"identifiers":1832},"10.1180\u002Fminmag.1971.038.295.09",{"doi":1831},{"id":24,"text":1834,"url":24,"identifiers":1835},"VANN I. R. 1978. The siting of Tertiary vulcanicity. Geol. J. Spec. Issue 10, 393–414.",{},{"id":24,"text":1837,"url":24,"identifiers":1838},"10.1016\u002F0016-7037(56)90024-2",{"doi":1837},{"id":24,"text":1840,"url":24,"identifiers":1841},"10.1038\u002F172068a0",{"doi":1840},{"id":24,"text":1843,"url":24,"identifiers":1844},"WAGER L. R., BROWN G. M. 1968. Layered igneous rocks, Oliver and Boyd.",{},{"id":24,"text":1846,"url":24,"identifiers":1847},"10.1180\u002Fminmag.1962.033.256.04",{"doi":1846},{"id":24,"text":1849,"url":24,"identifiers":1850},"WAGER L. R., VINCENT E. A., BROWN G. M., BELL J. D. 1965. Marscoite and related rocks of the Western Redhills Complex, Isle of Skye. Philos. Trans. R. Soc. Lond. A257, 273–307.",{"doi":1851},"10.1098\u002Frsta.1965.0006",{"id":24,"text":1853,"url":24,"identifiers":1854},"10.1130\u002F0016-7606(1976)87\u003C646:CHOLPB>2.0.CO;2",{"doi":1853},{"id":24,"text":1856,"url":24,"identifiers":1857},"10.1007\u002FBF00374440",{"doi":1856},{"id":24,"text":1859,"url":24,"identifiers":1860},"10.1180\u002Fminmag.1960.032.250.01",{"doi":1859},{"id":24,"text":1862,"url":24,"identifiers":1863},"WALKER G. P. L. 1970. The distribution of amygdale minerals in Mull and Morvern (western Scotland). In , Murty T. V. V. G. R. K., Rao S. S. (eds.), Studies in earth sciences (West Commem. Vol.), Univ. Saugar.",{},{"id":24,"text":1865,"url":24,"identifiers":1866},"10.1144\u002Fgsjgs.131.2.0121",{"doi":1865},{"id":24,"text":1868,"url":24,"identifiers":1869},"10.1016\u002F0012-8252(66)90024-9",{"doi":1868},{"id":24,"text":1871,"url":24,"identifiers":1872},"10.1007\u002FBF00375426",{"doi":1871},{"id":24,"text":1874,"url":24,"identifiers":1875},"10.1007\u002FBF00372849",{"doi":1874},{"id":24,"text":1877,"url":24,"identifiers":1878},"10.1016\u002F0012-821X(80)90214-9",{"doi":1877},{"id":24,"text":1880,"url":24,"identifiers":1881},"10.1016\u002F0012-821X(80)90211-3",{"doi":1880},{"id":24,"text":1883,"url":24,"identifiers":1884},"10.1029\u002FJB076i005p01171",{"doi":1883},{"id":24,"text":1886,"url":24,"identifiers":1887},"WILLIAMS S., MURTHY V. R. 1979. Sources and genetic relationships of volcanic rocks from the northern Rio Grande Rift: Rb-Sr and Sm-Nd evidence. EOS Trans. Am. Geophys. Union 60, 407.",{},{"id":24,"text":1889,"url":24,"identifiers":1890},"10.1016\u002F0016-7037(79)90092-9",{"doi":1889},{"id":24,"text":1892,"url":24,"identifiers":1893},"10.1016\u002F0012-821X(80)90116-8",{"doi":1892},{"id":24,"text":1895,"url":24,"identifiers":1896},"10.1007\u002FBF00371335",{"doi":1895},{"id":24,"text":1898,"url":24,"identifiers":1899},"10.1007\u002FBF00375360",{"doi":1898},{"id":24,"text":1901,"url":24,"identifiers":1902},"WOODHALL D., KNOX R. W. O'B. 1979. Mesozoic volcanism in the northern North Sea and adjacent areas. Bull. Geol. Surv. 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