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Subalkaline Rocks:A. Tholeiitic basalt series:Tholeiitic picrite-basalt; tholeiite; tholeiitic andesite.B. Calc-alkali series:High-alumina basalt; andesite; dacite; rhyolite.II. Alkaline Rocks:A. Alkali olivine basalt series:(1) Alkalic picrite–basalt; ankaramite; alkali basalt; hawaiite; mugearite; benmorite; trachyte.(2) Alkalic picrite–basalt; ankaramite; alkali basalt; trachybasalt; tristanite; trachyte.B. Nephelinic, leucitic, and analcitic rocks.III. Peralkaline Rocks:pantellerite, commendite, etc. \u003C\u002Fjats:p>",{"EN":102,"VI":103},"A Guide to the Chemical Classification of the Common Volcanic Rocks","Hướng dẫn phân loại hoá học các đá núi lửa thông thường",{"VOID":105},"10.1139\u002Fe71-055","PUBLICATION","Author affiliation is blank",[109],"EN",[111],"VI","http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe71-055",[114,123],{"id":115,"sortIndex":25,"researcher":24,"roles":116,"affiliations":117,"properties":118,"displayName":120,"givenName":24,"familyName":24},"d45fd462-cf6a-409d-a9e3-2a4825f75be3",[],[],{"title":119,"openalex":121},{"EN":120},"Τ. N. 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Plant taxa from these fossil sites are characteristic of the modern eastern North American deciduous forest zone, principally the mixed mesophytic forest, but also include extinct taxa, taxa known only from eastern Asian mesothermal forests, and a small number of taxa restricted to the present-day North American west coast coniferous biome. In this preliminary report, paleoclimates and forest types are reconstructed using collections from Republic in Washington State, USA., and Princeton, Quilchena, Falkland, McAbee, Hat Creek, Horsefly, and Driftwood Canyon in British Columbia, Canada. Both leaf margin analysis (LMA) and quantitative bioclimatic analysis of identified nearest living relatives of megaflora indicated upper microthermal to lower mesothermal moist environments (MAT ~10–15 °C, CMMT > 0 °C, MAP > 100 cm\u002Fyear). Some taxa common to most sites suggest cool conditions (e.g., Abies, other Pinaceae; Alnus, other Betulaceae). However, all floras contain a substantive broadleaf deciduous element (e.g., Fagaceae, Juglandaceae) and conifers (e.g., Metasequoia) with the bioclimatic analysis yielding slightly higher MAT than LMA. Thermophilic (principally mesothermal) taxa include various insects, the aquatic fern Azolla, palms, the banana relative Ensete, taxodiaceous conifers, Eucommia and Gordonia, taxa which may have occurred near their climatic limits. 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Review of Palaeobotany and Palynology, 81, 83, 10.1016\u002F0034-6667(94)90128-7",{"doi":435},"10.1016\u002F0034-6667(94)90128-7",{"id":24,"text":437,"url":24,"identifiers":438},"Greenwood D.R., 1995, Geology, 23, 1040, 10.1130\u002F0091-7613(1995)023\u003C1044:ECCALT>2.3.CO;2",{"doi":439},"10.1130\u002F0091-7613(1995)023\u003C1044:ECCALT>2.3.CO;2",{"id":24,"text":441,"url":24,"identifiers":442},"Greenwood D.R., 2003, Thomas. Geological Society of America Special Paper, 369, 365",{},{"id":24,"text":444,"url":24,"identifiers":445},"Heie O.E., 1967, Spoia Zoologica Musei Hauniensis, 26, 1",{},{"id":24,"text":447,"url":24,"identifiers":448},"Heie O.E., 1994, European Journal of Entomology, 91, 127",{},{"id":24,"text":450,"url":24,"identifiers":451},"Hopkins D.J., 1997, Washington Geology, 25, 37",{},{"id":24,"text":453,"url":24,"identifiers":454},"Janzen D.H., 1981, Ecology, 62, 532, 10.2307\u002F1937717",{"doi":455},"10.2307\u002F1937717",{"id":24,"text":457,"url":24,"identifiers":458},"Johnson K.R., 1996, Washington Geology, 24, 41",{},{"id":24,"text":460,"url":24,"identifiers":461},"Kershaw A.P., 1996, Australian Journal of Botany, 45, 373, 10.1071\u002FBT96033",{"doi":462},"10.1071\u002FBT96033",{"id":24,"text":464,"url":24,"identifiers":465},"Kershaw A.P., 1988, Journal of Biogeography, 15, 589, 10.2307\u002F2845438",{"doi":466},"10.2307\u002F2845438",{"id":24,"text":468,"url":24,"identifiers":469},"Kingsolver J.M., 1965, Coleopterists' Bulletin, 19, 25",{},{"id":24,"text":471,"url":24,"identifiers":472},"Lewis S.E., 1992, Washington. Washington Geology, 20, 15",{},{"id":24,"text":474,"url":24,"identifiers":475},"Manchester S.R., 1999, Annals of the Missouri Botanical Gardens, 86, 472, 10.2307\u002F2666183",{"doi":476},"10.2307\u002F2666183",{"id":24,"text":478,"url":24,"identifiers":479},"Makarkin V.N., 2003, The Canadian Entomologist, 135, 637, 10.4039\u002Fn02-122",{"doi":480},"10.4039\u002Fn02-122",{"id":24,"text":482,"url":24,"identifiers":483},"Markwick P.J., 1994, Geology, 22, 613, 10.1130\u002F0091-7613(1994)022\u003C0613:ECATCT>2.3.CO;2",{"doi":484},"10.1130\u002F0091-7613(1994)022\u003C0613:ECATCT>2.3.CO;2",{"id":24,"text":486,"url":24,"identifiers":487},"Mathewes R.W., 1971, Syesis, 4, 209",{},{"id":24,"text":489,"url":24,"identifiers":490},"McAndrews J.H., 1969, Review of Palaeobotany and Palynology, 9, 17, 10.1016\u002F0034-6667(69)90011-6",{"doi":491},"10.1016\u002F0034-6667(69)90011-6",{"id":24,"text":493,"url":24,"identifiers":494},"McClain A.M., 2001, American Journal of Botany, 88, 1316, 10.2307\u002F3558343",{"doi":495},"10.2307\u002F3558343",{"id":24,"text":497,"url":24,"identifiers":498},"Mosbrugger V., 1997, Palaeoecology, 134, 61, 10.1016\u002FS0031-0182(96)00154-X",{"doi":499},"10.1016\u002FS0031-0182(96)00154-X",{"id":24,"text":501,"url":24,"identifiers":502},"Moss P.T., 2000, Palaeoecology, 155, 155, 10.1016\u002FS0031-0182(99)00099-1",{"doi":503},"10.1016\u002FS0031-0182(99)00099-1",{"id":24,"text":505,"url":24,"identifiers":506},"Moss P.T., 2005, Canadian Journal of Earth Sciences, 42: This issue.",{},{"id":24,"text":508,"url":24,"identifiers":509},"Mustoe G.E., 2002, Washington Geology, 30, 17",{},{"id":24,"text":511,"url":24,"identifiers":512},"Pigg K.B., 1994, Washington Geology, 22, 32",{},{"id":24,"text":514,"url":24,"identifiers":515},"Pigg K.B., 2002, Washington Geology, 30, 3",{},{"id":24,"text":517,"url":24,"identifiers":518},"Pigg K.B., 2003, International Journal of Plant Sciences, 164, 807, 10.1086\u002F376816",{"doi":519},"10.1086\u002F376816",{"id":24,"text":521,"url":24,"identifiers":522},"Poinar G.O., Jr., 1999, The Canadian Entomologist, 131, 171, 10.4039\u002FEnt131171-2",{"doi":523},"10.4039\u002FEnt131171-2",{"id":24,"text":525,"url":24,"identifiers":526},"Rice H.M.A., 1959, Bulletin, 55, 1",{},{"id":24,"text":528,"url":24,"identifiers":529},"Rouse G.E., 1971, Special Paper, 127, 213",{},{"id":24,"text":531,"url":24,"identifiers":532},"Royer D.L., 2002, Geology, 30, 963, 10.1130\u002F0091-7613(2002)030\u003C0963:HCITFS>2.0.CO;2",{"doi":533},"10.1130\u002F0091-7613(2002)030\u003C0963:HCITFS>2.0.CO;2",{"id":24,"text":535,"url":24,"identifiers":536},"Russell L.S., 1935, American Journal of Science, 29, 54, 10.2475\u002Fajs.s5-29.169.54",{"doi":537},"10.2475\u002Fajs.s5-29.169.54",{"id":24,"text":539,"url":24,"identifiers":540},"Schorn H.E., 1994, Washington. Washington Geology, 22, 22",{},{"id":24,"text":542,"url":24,"identifiers":543},"Scudder S.H., 1879, Report of Progress of the Geological Survey of Canada, 1877, 176B",{},{"id":24,"text":545,"url":24,"identifiers":546},"Spicer R.A., 1987, Paleobiology, 13, 227, 10.1017\u002FS0094837300008770",{"doi":547},"10.1017\u002FS0094837300008770",{"id":24,"text":549,"url":24,"identifiers":550},"Stockey R.A., 1998, Review of Palaeobotany and Palynology, 103, 223, 10.1016\u002FS0034-6667(98)00038-4",{"doi":551},"10.1016\u002FS0034-6667(98)00038-4",{"id":24,"text":553,"url":24,"identifiers":554},"Steart D.C., 2002, Archiv für Hydrobiologie, 156, 43, 10.1127\u002F0003-9136\u002F2002\u002F0156-0043",{"doi":555},"10.1127\u002F0003-9136\u002F2002\u002F0156-0043",{"id":24,"text":557,"url":24,"identifiers":558},"Thompson R.S., 1999, Online Version, 1, 1999",{},{"id":24,"text":560,"url":24,"identifiers":561},"Tribe S., 2005, Canadian Journal of Earth Sciences, 42: This issue.",{},{"id":24,"text":563,"url":24,"identifiers":564},"Wehr W.C., 1998, Report, 6, 99",{},{"id":24,"text":566,"url":24,"identifiers":567},"Wehr W.C., 1996, Washington. Washington Geology, 24, 25",{},{"id":24,"text":569,"url":24,"identifiers":570},"Wilf P., 1997, Paleobiology, 23, 373, 10.1017\u002FS0094837300019746",{"doi":571},"10.1017\u002FS0094837300019746",{"id":24,"text":573,"url":24,"identifiers":574},"Wilf P., 2003, Science, 300, 122, 10.1126\u002Fscience.1080475",{"doi":575},"10.1126\u002Fscience.1080475",{"id":24,"text":577,"url":24,"identifiers":578},"Wilson M.V.H., 1977, Canadian Journal of Earth Science, 14, 1139, 10.1139\u002Fe77-104",{"doi":579},"10.1139\u002Fe77-104",{"id":24,"text":581,"url":24,"identifiers":582},"Wilson M.V.H., 1977, Life Sciences Contributions 113, Royal Ontario Museum, Toronto, Ont., 1",{},{"id":24,"text":584,"url":24,"identifiers":585},"Wilson M.V.H., 1977, Canadian Journal of Earth Science, 14, 953, 10.1139\u002Fe77-089",{"doi":586},"10.1139\u002Fe77-089",{"id":24,"text":588,"url":24,"identifiers":589},"Wilson M.V.H., 1980, Palaeoecology, 32, 21, 10.1016\u002F0031-0182(80)90029-2",{"doi":590},"10.1016\u002F0031-0182(80)90029-2",{"id":24,"text":592,"url":24,"identifiers":593},"Wilson M.V.H., 1987, Palaios, 2, 497, 10.2307\u002F3514620",{"doi":594},"10.2307\u002F3514620",{"id":24,"text":596,"url":24,"identifiers":597},"Wolfe J.A., 1979, US. Geological Survey Professional Paper, 1106, 1",{},{"id":24,"text":599,"url":24,"identifiers":600},"Wolfe J.A., 1985, Geophysical Monograph, 32, 357",{},{"id":24,"text":602,"url":24,"identifiers":603},"Wolfe J.A., 1987, Annals of the Missouri Botanical Gardens, 74, 785, 10.2307\u002F2399450",{"doi":604},"10.2307\u002F2399450",{"id":24,"text":606,"url":24,"identifiers":607},"Wolfe J.A., 1994, Palaeoecology, 108, 195, 10.1016\u002F0031-0182(94)90233-X",{"doi":608},"10.1016\u002F0031-0182(94)90233-X",{"id":24,"text":610,"url":24,"identifiers":611},"Wolfe J.A., 1987, US. Geological Survey Bulletin, 1597, 1",{},{"id":24,"text":613,"url":24,"identifiers":614},"Wolfe J.A., 1998, Geological Society of America Bulletin, 110, 664, 10.1130\u002F0016-7606(1998)110\u003C0664:PEOEAO>2.3.CO;2",{"doi":615},"10.1130\u002F0016-7606(1998)110\u003C0664:PEOEAO>2.3.CO;2",{"id":24,"text":617,"url":24,"identifiers":618},"Zachos J.C., 2001, Science, 292, 686, 10.1126\u002Fscience.1059412",{"doi":619},"10.1126\u002Fscience.1059412",{"id":621,"createTime":622,"updateTime":622,"relativeEntities":623,"slug":624,"properties":625,"entityType":106,"verifyStatus":23,"verifyTime":636,"verifyNote":107,"languages":637,"translateLanguages":24,"viewCount":25,"primaryUrl":638,"fullTextUrl":24,"authors":639,"publicationType":133,"publisherRelationship":658,"citationCount":703,"citationInfo":704,"publishDate":707,"publishYear":705,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":708,"openAccess":24,"references":709,"isForceReanalyzing":200},"a3f9caeb-2c5a-44c9-a1d2-449d03211398","2024-12-20T23:09:57.003+00:00",[],"A-study-of-the-isotopic-abundance-of-boron-from-various-sources",{"openalex":626,"mag":628,"abstract":630,"title":632,"doi":634},{"VOID":627},"W2072464842",{"VOID":629},"2072464842",{"EN":631},"\u003Cjats:p> The absolute ratio of \u003Cjats:sup>11\u003C\u002Fjats:sup>B\u002F\u003Cjats:sup>10\u003C\u002Fjats:sup>B has been determined for boron from different terrestrial sources with a precision of 0.2% (two standard errors) and a reproducibility of 0.2% (half-range). Values fall in the range 4.108 to 3.987 (i.e. 3% variation) and give a corresponding range in the boron atomic weight of 10.814 to 10.810 (0.04% variation). The absolute ratios are 7% lower than those reported by early workers, but are in accord with the results of recent investigations. Igneous rocks and boric acid are found to have high isotopic ratios, whereas Tokyo Bay water possesses a value for \u003Cjats:sup>11\u003C\u002Fjats:sup>B\u002F\u003Cjats:sup>10\u003C\u002Fjats:sup>B near the mean. \u003C\u002Fjats:p>",{"EN":633},"A study of the isotopic abundance of boron from various sources",{"VOID":635},"10.1139\u002Fe68-088","2024-12-20T23:09:56.998+00:00",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe68-088",[640,649],{"id":641,"sortIndex":25,"researcher":24,"roles":642,"affiliations":643,"properties":644,"displayName":646,"givenName":24,"familyName":24},"ec32ceee-70c0-4bae-9b39-5b78dd4e37ad",[],[],{"title":645,"openalex":647},{"EN":646},"EK Agyei",{"VOID":648},"A5057792494",{"id":650,"sortIndex":125,"researcher":24,"roles":651,"affiliations":652,"properties":653,"displayName":655,"givenName":24,"familyName":24},"00e0fae6-f317-446c-9f1e-e6b9736cfe79",[],[],{"title":654,"openalex":656},{"EN":655},"C. C. McMullen",{"VOID":657},"A5087389682",{"url":24,"publisher":659,"properties":697},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":660,"slug":10,"properties":661,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":666,"manageAffiliations":671,"indexDatabases":682,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":662,"eissn":663,"issn":664,"title":665},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[667],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":668,"label":669,"description":670,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[672,677],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":673,"slug":24,"properties":674,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":676,"statistic":24},[],{"title":675},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":678,"slug":24,"properties":679,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":681,"statistic":24},[],{"title":680},{"EN":46},[],[683,690],{"id":67,"indexDatabase":684,"url":78,"indexYears":79,"academicFieldIds":689,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":685,"label":686,"description":687,"key":75,"publicationTags":688,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"id":50,"indexDatabase":691,"url":63,"indexYears":24,"academicFieldIds":696,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":692,"label":693,"description":694,"key":59,"publicationTags":695,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"issue":698,"pages":700,"volume":702},{"VOID":699},"4",{"VOID":701},"921-927",{"VOID":175},41,{"total":703,"publishYear":705,"statisticByYear":706},1968,{"2014":125,"2016":262,"2017":262},"1968-08-01",[61,82],[],{"id":711,"createTime":712,"updateTime":712,"relativeEntities":713,"slug":714,"properties":715,"entityType":106,"verifyStatus":23,"verifyTime":712,"verifyNote":107,"languages":726,"translateLanguages":24,"viewCount":25,"primaryUrl":727,"fullTextUrl":24,"authors":728,"publicationType":133,"publisherRelationship":740,"citationCount":786,"citationInfo":787,"publishDate":800,"publishYear":788,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":801,"openAccess":24,"references":802,"isForceReanalyzing":200},"1fc3a1e8-e3b3-4e28-beec-199fe8926efb","2024-12-17T08:16:20.523+00:00",[],"U-Pb-dating-of-monazite-and-its-application-to-geological-problems",{"openalex":716,"mag":718,"abstract":720,"title":722,"doi":724},{"VOID":717},"W2091184061",{"VOID":719},"2091184061",{"EN":721},"\u003Cjats:p> Monazite is an underutilized mineral in U–Pb geochronological studies of crustal rocks. It occurs as an accessory mineral in a wide variety of rocks, including granite, pegmatite, felsic volcanic ash, felsic gneiss, pelitic schist and gneiss of medium to high metamorphic grade, and low-grade metasedimentary rocks, and as a detrital mineral in clastic and metaclastic sediments.In geochronological applications, it can be used to date the crystallization of igneous rocks, determine the age of metamorphism in metamorphic rocks of variable metamorphic grade, and determine the age and neodymium isotopic characteristics of source materials of both igneous and sedimentary rocks. It is particularly useful in the dating of peraluminous granitic rocks where zircon inheritance often precludes a precise U–Pb age for magmatic zircon. The U–Pb systematics of the mineral are not without complexity, however. Being a mineral that favors incorporation of Th relative to U, it can contain considerable amounts of excess \u003Cjats:sup>206\u003C\u002Fjats:sup>Pb derived from initially incorporated \u003Cjats:sup>230\u003C\u002Fjats:sup>Th, an intermediate decay product of \u003Cjats:sup>238\u003C\u002Fjats:sup>U. Corrections for this effect can be made using the Th\u002FU ratio of the host rock, but these corrections may not always be valid. Monazite is known to be capable of preserving inheritance in a manner similar to that of zircon, and it can lose Pb during episodic or prolonged heating events of uppermost amphibolite and granulite facies metamorphic grades. Monazite is less retentive of Pb than zircon during high-temperature igneous and metamorphic processes, and a few studies of its behavior suggest that its closure temperature is approximately 725 ± 25 °C. Examples of U–Pb systematics from most of the above situations are presented in this paper to illustrate both the utility and complexity of monazite in geochronological studies in an attempt to encourage more widespread application of this dating method. \u003C\u002Fjats:p>",{"EN":723},"U–Pb dating of monazite and its application to geological problems",{"VOID":725},"10.1139\u002Fe90-152",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe90-152",[729],{"id":730,"sortIndex":25,"researcher":24,"roles":731,"affiliations":732,"properties":733,"displayName":737,"givenName":24,"familyName":24},"7f6cd13c-bc70-45c6-b7e4-a1009c3126f3",[],[],{"orcid":734,"title":736,"openalex":738},{"VOID":735},"https:\u002F\u002Forcid.org\u002F0000-0001-6801-8379",{"EN":737},"Randall R. Parrish",{"VOID":739},"A5053950525",{"url":24,"publisher":741,"properties":779},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":742,"slug":10,"properties":743,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":748,"manageAffiliations":753,"indexDatabases":764,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":744,"eissn":745,"issn":746,"title":747},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[749],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":750,"label":751,"description":752,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[754,759],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":755,"slug":24,"properties":756,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":758,"statistic":24},[],{"title":757},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":760,"slug":24,"properties":761,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":763,"statistic":24},[],{"title":762},{"EN":46},[],[765,772],{"id":67,"indexDatabase":766,"url":78,"indexYears":79,"academicFieldIds":771,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":767,"label":768,"description":769,"key":75,"publicationTags":770,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"id":50,"indexDatabase":773,"url":63,"indexYears":24,"academicFieldIds":778,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":774,"label":775,"description":776,"key":59,"publicationTags":777,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"issue":780,"pages":782,"volume":784},{"VOID":781},"11",{"VOID":783},"1431-1450",{"VOID":785},"27",914,{"total":786,"publishYear":788,"statisticByYear":789},1990,{"2012":790,"2013":791,"2014":790,"2015":792,"2016":793,"2017":794,"2018":795,"2019":796,"2020":793,"2021":797,"2022":798,"2023":799,"2024":793},33,28,29,25,40,21,31,30,24,34,"1990-11-01",[61,82],[],{"id":804,"createTime":805,"updateTime":805,"relativeEntities":806,"slug":807,"properties":808,"entityType":106,"verifyStatus":217,"verifyTime":805,"verifyNote":218,"languages":819,"translateLanguages":24,"viewCount":25,"primaryUrl":820,"fullTextUrl":24,"authors":821,"publicationType":133,"publisherRelationship":925,"citationCount":971,"citationInfo":972,"publishDate":979,"publishYear":973,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":980,"openAccess":24,"references":981,"isForceReanalyzing":200},"a06b9d2e-5935-4a08-89c2-04caeb0aab99","2024-12-12T13:49:12.746+00:00",[],"Tectonic-evolution-of-the-western-Superior-Province-from-NATMAP-and-Lithoprobe-studies",{"openalex":809,"mag":811,"abstract":813,"title":815,"doi":817},{"VOID":810},"W2057731022",{"VOID":812},"2057731022",{"EN":814},"\u003Cjats:p> Five discrete accretionary events assembled fragments of continental and oceanic crust into a coherent Superior craton by 2.60 Ga. They exhibit similar sequences of events at ~10 million year intervals: cessation of arc magmatism, early deformation, synorogenic sedimentation, sanukitoid magmatism, bulk shortening, regional metamorphism, late transpression, orogenic gold localization, emplacement of crust-derived granites, and postorogenic cooling. The Northern Superior superterrane recorded 3.7–2.75 Ga events prior to 2.72 Ga collision with the 3.0 Ga North Caribou superterrane. Following 2.98 Ga rifting, the Uchi margin of the North Caribou superterrane evolved in an upper plate setting before 2.72–2.70 Ga collision of the <3.4 Ga Winnipeg River terrane, which trapped synorogenic English River turbidites in the collision zone. The Winnipeg River terrane was reworked in 2.75–2.68 Ga magmatic and tectonic events, including the central Superior orogeny (2.71–2.70 Ga) that marks accretion of the juvenile western Wabigoon terrane. In the south, the Wawa–Abitibi terrane evolved in a mainly oceanic setting until Shebandowanian collision with the composite Superior superterrane at 2.695 Ga. Synorogenic Quetico turbidites were trapped in the collision zone. The final accretionary event involved addition of the Minnesota River Valley terrane (MRVT) from the south, and deposition and metamorphism of synorogenic turbidites of the Pontiac terrane during the ~2.68 Ga Minnesotan orogeny. Seismic reflection and refraction images indicate north-dipping structures, interpreted as a stack of discrete 10–15 km thick terranes. A slab of high-velocity material, possibly representing subcreted oceanic lithosphere, as well as Moho offsets, support a model of progressive accretion through plate-tectonic-like processes. \u003C\u002Fjats:p>",{"EN":816},"Tectonic evolution of the western Superior Province from NATMAP and Lithoprobe studies",{"VOID":818},"10.1139\u002Fe06-062",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe06-062",[822,839,856,873,890,908],{"id":823,"sortIndex":25,"researcher":24,"roles":824,"affiliations":825,"properties":834,"displayName":836,"givenName":24,"familyName":24},"e5126abf-13ab-4735-b398-c3e8d0032a0e",[],[826],{"id":827,"sortIndex":25,"affiliation":828,"properties":24},"20dc6f9e-f019-419e-99dc-306a5ed6ddcc",{"id":827,"createTime":24,"updateTime":24,"relativeEntities":829,"slug":24,"properties":830,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":833,"statistic":24},[],{"title":831},{"VI":832},"Geological Survey of Canada, 601 Booth Street, Ottawa, ON K1A 0E8, Canada",[],{"title":835,"openalex":837},{"EN":836},"J A Percival",{"VOID":838},"A5109146302",{"id":840,"sortIndex":125,"researcher":24,"roles":841,"affiliations":842,"properties":849,"displayName":853,"givenName":24,"familyName":24},"85737b06-e865-486a-9862-89c2ceaf84b2",[],[843],{"id":827,"sortIndex":25,"affiliation":844,"properties":24},{"id":827,"createTime":24,"updateTime":24,"relativeEntities":845,"slug":24,"properties":846,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":848,"statistic":24},[],{"title":847},{"VI":832},[],{"orcid":850,"title":852,"openalex":854},{"VOID":851},"https:\u002F\u002Forcid.org\u002F0000-0001-6138-4990",{"EN":853},"M Sanborn-Barrie",{"VOID":855},"A5027250248",{"id":857,"sortIndex":262,"researcher":24,"roles":858,"affiliations":859,"properties":866,"displayName":870,"givenName":24,"familyName":24},"00c10600-b532-4051-a139-d5de0454ae9b",[],[860],{"id":827,"sortIndex":25,"affiliation":861,"properties":24},{"id":827,"createTime":24,"updateTime":24,"relativeEntities":862,"slug":24,"properties":863,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":865,"statistic":24},[],{"title":864},{"VI":832},[],{"orcid":867,"title":869,"openalex":871},{"VOID":868},"https:\u002F\u002Forcid.org\u002F0000-0002-8311-1464",{"EN":870},"T Skulski",{"VOID":872},"A5020886559",{"id":874,"sortIndex":282,"researcher":24,"roles":875,"affiliations":876,"properties":885,"displayName":887,"givenName":24,"familyName":24},"6e2f4c99-29d6-4846-a1a3-aacea46eee4a",[],[877],{"id":878,"sortIndex":25,"affiliation":879,"properties":24},"055369dc-97de-4dcb-b4e6-41c80bbb0c81",{"id":878,"createTime":24,"updateTime":24,"relativeEntities":880,"slug":24,"properties":881,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":884,"statistic":24},[],{"title":882},{"VI":883},"Ontario Geological Survey, 933 Ramsey Lake Road, Sudbury, ON, P3E 6B5, Canada",[],{"title":886,"openalex":888},{"EN":887},"G. 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10.1130\u002F0016-7606(1991)103\u003C1385:OTGOAG>2.3.CO;2",{"doi":1554},"10.1130\u002F0016-7606(1991)103\u003C1385:OTGOAG>2.3.CO;2",{"id":24,"text":1556,"url":24,"identifiers":1557},"Stern R.A., 1991, Journal of Petrology, 32, 201, 10.1093\u002Fpetrology\u002F32.1.201",{"doi":1558},"10.1093\u002Fpetrology\u002F32.1.201",{"id":24,"text":1560,"url":24,"identifiers":1561},"Stern R.A., 1989, Canadian Journal of Earth Sciences, 26, 1688, 10.1139\u002Fe89-145",{"doi":1562},"10.1139\u002Fe89-145",{"id":24,"text":1564,"url":24,"identifiers":1565},"Stevenson R.K., 1995, Geological Society of America Bulletin, 107, 1458, 10.1130\u002F0016-7606(1995)107\u003C1458:CAMEIT>2.3.CO;2",{"doi":1566},"10.1130\u002F0016-7606(1995)107\u003C1458:CAMEIT>2.3.CO;2",{"id":24,"text":1568,"url":24,"identifiers":1569},"Stevenson R.K., 1990, Geochimica et Cosmochimica Acta, 54, 1683, 10.1016\u002F0016-7037(90)90400-F",{"doi":1570},"10.1016\u002F0016-7037(90)90400-F",{"id":24,"text":1572,"url":24,"identifiers":1573},"Stevenson R.K., 1992, Canadian Journal of Earth Sciences, 29, 2200, 10.1139\u002Fe92-174",{"doi":1574},"10.1139\u002Fe92-174",{"id":24,"text":1576,"url":24,"identifiers":1577},"Stevenson R., 1999, Precambrian Research, 96, 83, 10.1016\u002FS0301-9268(99)00009-1",{"doi":1578},"10.1016\u002FS0301-9268(99)00009-1",{"id":24,"text":1580,"url":24,"identifiers":1581},"Stevenson R.K., 2000, Lithoprobe Report, 77, 116",{},{"id":24,"text":1583,"url":24,"identifiers":1584},"Stone D., 2000, Canadian Mineralogist, 38, 455, 10.2113\u002Fgscanmin.38.2.455",{"doi":1585},"10.2113\u002Fgscanmin.38.2.455",{"id":24,"text":1587,"url":24,"identifiers":1588},"Stott G.M., 2000, Open File Report, 6032, 14",{},{"id":24,"text":1590,"url":24,"identifiers":1591},"Stott G.M., 1991, Special, 4, 1. pp. 145",{},{"id":24,"text":1593,"url":24,"identifiers":1594},"Thurston P.C., 2002, Precambrian Research, 115, 11, 10.1016\u002FS0301-9268(02)00004-9",{"doi":1595},"10.1016\u002FS0301-9268(02)00004-9",{"id":24,"text":1597,"url":24,"identifiers":1598},"Thurston P.C., 1990, Precambrian Research, 46, 21, 10.1016\u002F0301-9268(90)90065-X",{"doi":1599},"10.1016\u002F0301-9268(90)90065-X",{"id":24,"text":1601,"url":24,"identifiers":1602},"Thurston P.C., 1985, Miscellaneous Paper, 126, 138",{},{"id":24,"text":1604,"url":24,"identifiers":1605},"Thurston P.C., 1991, Special, 4, 1. pp. 81",{},{"id":24,"text":1607,"url":24,"identifiers":1608},"Tomlinson K.Y., 2003, Open File Report, 6120, 13",{},{"id":24,"text":1610,"url":24,"identifiers":1611},"Tomlinson K.Y., 1996, Canadian Journal of Earth Sciences, 33, 1520, 10.1139\u002Fe96-115",{"doi":1612},"10.1139\u002Fe96-115",{"id":24,"text":1614,"url":24,"identifiers":1615},"Tomlinson K.Y., 1998, Precambrian Research, 89, 59, 10.1016\u002FS0301-9268(97)00078-8",{"doi":1616},"10.1016\u002FS0301-9268(97)00078-8",{"id":24,"text":1618,"url":24,"identifiers":1619},"Tomlinson K.Y., 2002, Precambrian Research, 114, 295, 10.1016\u002FS0301-9268(01)00232-7",{"doi":1620},"10.1016\u002FS0301-9268(01)00232-7",{"id":24,"text":1622,"url":24,"identifiers":1623},"Tomlinson K.Y., 2004, Precambrian Research, 132, 245, 10.1016\u002Fj.precamres.2003.12.017",{"doi":1624},"10.1016\u002Fj.precamres.2003.12.017",{"id":24,"text":1626,"url":24,"identifiers":1627},"Turek A., 1986, Canadian Journal of Earth Sciences, 23, 92, 10.1139\u002Fe86-009",{"doi":1628},"10.1139\u002Fe86-009",{"id":24,"text":1630,"url":24,"identifiers":1631},"Turek A., 1992, Canadian Journal of Earth Sciences, 29, 1154, 10.1139\u002Fe92-093",{"doi":1632},"10.1139\u002Fe92-093",{"id":24,"text":1634,"url":24,"identifiers":1635},"Ueda H., 2001, Journal of the Geological Society of Japan, 107, 81, 10.5575\u002Fgeosoc.107.81",{"doi":1636},"10.5575\u002Fgeosoc.107.81",{"id":24,"text":1638,"url":24,"identifiers":1639},"Valli F., 2004, Precambrian Research, 132, 155, 10.1016\u002Fj.precamres.2004.03.002",{"doi":1640},"10.1016\u002Fj.precamres.2004.03.002",{"id":24,"text":1642,"url":24,"identifiers":1643},"Van der Lee S., 1997, Journal of Geophysical Research, 102, 815, 10.1029\u002F97JB01168",{"doi":1644},"10.1029\u002F97JB01168",{"id":24,"text":1646,"url":24,"identifiers":1647},"van Staal C.R., 1998, Blundell and A.C. Scott. Geological Society Special Publication, 143, 199",{},{"id":24,"text":1649,"url":24,"identifiers":1650},"Vicker P.A., 1994, Mineralogical Association of Canada Program with Abstracts, 19, 116",{},{"id":24,"text":1652,"url":24,"identifiers":1653},"Vroon P.Z., 1993, Journal of Geophysical Research, 98, 349, 10.1029\u002F93JB01716",{"doi":1654},"10.1029\u002F93JB01716",{"id":24,"text":1656,"url":24,"identifiers":1657},"Whalen J.B., 2002, Journal of Petrology, 43, 1551, 10.1093\u002Fpetrology\u002F43.8.1551",{"doi":1658},"10.1093\u002Fpetrology\u002F43.8.1551",{"id":24,"text":1660,"url":24,"identifiers":1661},"Whalen J.B., 2004, Precambrian Research, 132, 303, 10.1016\u002Fj.precamres.2003.11.007",{"doi":1662},"10.1016\u002Fj.precamres.2003.11.007",{"id":24,"text":1664,"url":24,"identifiers":1665},"Whalen J.B., 2004, Precambrian Research, 132, 275, 10.1016\u002Fj.precamres.2004.02.008",{"doi":1666},"10.1016\u002Fj.precamres.2004.02.008",{"id":24,"text":1668,"url":24,"identifiers":1669},"White D.J., 2003, Geology, 31, 997, 10.1130\u002FG20014.1",{"doi":1670},"10.1130\u002FG20014.1",{"id":24,"text":1672,"url":24,"identifiers":1673},"Williams H.R., 1991, Special, 4, 1. pp. 383",{},{"id":24,"text":1675,"url":24,"identifiers":1676},"Williams H.R., 1991, Special, 4, 1. pp. 485",{},{"id":24,"text":1678,"url":24,"identifiers":1679},"Williams H.R., 1992, Special, 4, 2. pp. 1255",{},{"id":24,"text":1681,"url":24,"identifiers":1682},"Wyman D., 2000, Earth and Planetary Science Letters, 179, 21, 10.1016\u002FS0012-821X(00)00106-0",{"doi":1683},"10.1016\u002FS0012-821X(00)00106-0",{"id":24,"text":1685,"url":24,"identifiers":1686},"Zaleski E., 1999, Canadian Journal of Earth Sciences, 36, 945, 10.1139\u002Fe99-016",{"doi":1687},"10.1139\u002Fe99-016",{"id":24,"text":1689,"url":24,"identifiers":1690},"Zweng P.L., 1993, Economic Geology, 88, 1700, 10.2113\u002Fgsecongeo.88.6.1700",{"doi":1691},"10.2113\u002Fgsecongeo.88.6.1700",{"id":1693,"createTime":1694,"updateTime":1694,"relativeEntities":1695,"slug":1696,"properties":1697,"entityType":106,"verifyStatus":23,"verifyTime":1708,"verifyNote":107,"languages":1709,"translateLanguages":24,"viewCount":25,"primaryUrl":1710,"fullTextUrl":24,"authors":1711,"publicationType":133,"publisherRelationship":1730,"citationCount":1775,"citationInfo":1776,"publishDate":1779,"publishYear":1777,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":1780,"openAccess":24,"references":1781,"isForceReanalyzing":200},"37ef56b1-0a20-4ba2-9649-8980ef2c3cf8","2024-12-12T13:49:08.515+00:00",[],"Oxygen-Isotope-Studies-of-Fresh-and-Weathered-Submarine-Basalts",{"openalex":1698,"mag":1700,"abstract":1702,"title":1704,"doi":1706},{"VOID":1699},"W2132429552",{"VOID":1701},"2132429552",{"EN":1703},"\u003Cjats:p> The \u003Cjats:sup>18\u003C\u002Fjats:sup>O\u002F\u003Cjats:sup>16\u003C\u002Fjats:sup>O ratios of fresh unmetamorphosed basalts from the Reykjanes, Mid-Atlantic, and Gorda Ridges and the East Pacific Rise fall in a narrow range of 5.5–5.9‰ (SMOW), identical to those of basalts from oceanic islands. Large plagioclase xenocrysts in some of the basalts are not in isotopic equilibrium with coexisting olivine. The basalts react with sea water at the ambient sea-floor temperature to form clays, resulting in an increase in δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O of the basalt of 0.25‰ per m.y. This provides a very sensitive method to detect early stages of weathering, which otherwise might go unnoticed. Advanced submarine weathering of basalt can remove nearly one half of its SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>, MgO, CaO, and Na\u003Cjats:sub>2\u003C\u002Fjats:sub>O and lesser amounts of Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>s\u003C\u002Fjats:sub> and TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>. Weathering does not proceed deeply enough into the basaltic sea floor to affect the chemical composition of sea water. Since it is likely that large amounts of basaltic debris (less than a few cm in radius) are on the ocean floor, their weathering can affect the ocean-sediment budget of TiO\u003Cjats:sub>2\u003C\u002Fjats:sub>, Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>, SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>, MgO, and CaO. \u003C\u002Fjats:p>",{"EN":1705},"Oxygen Isotope Studies of Fresh and Weathered Submarine Basalts",{"VOID":1707},"10.1139\u002Fe72-014","2024-12-12T13:49:08.514+00:00",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe72-014",[1712,1721],{"id":1713,"sortIndex":25,"researcher":24,"roles":1714,"affiliations":1715,"properties":1716,"displayName":1718,"givenName":24,"familyName":24},"1b0488c5-713a-4e0e-9b4a-2c33eff80b31",[],[],{"title":1717,"openalex":1719},{"EN":1718},"Karlis Muehlenbachs",{"VOID":1720},"A5061580951",{"id":1722,"sortIndex":125,"researcher":24,"roles":1723,"affiliations":1724,"properties":1725,"displayName":1727,"givenName":24,"familyName":24},"a51dfba2-6c00-4f2c-921c-b8e360325509",[],[],{"title":1726,"openalex":1728},{"EN":1727},"Robert N. 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Volcanically active island arcs to the south (Wawa subprovince) were transported northward during this interval and at ~2690 Ma collided with the accretionary complex (Quetico subprovince). Metamorphosed sedimentary units intercalated with the ocean floor and island-arc volcanic rocks of northern Wawa subprovince provided the opportunity to amass data useful in extending the paleogeographic interpretation of the area. This study examines the McKellar Harbour Formation, a several kilometre thick assemblage of graded metasandstone beds outcropping to the north of Lake Superior. Its sedimentology, geochemistry, and detrital U–Pb zircon geochronology were investigated in conjunction with the same attributes of possible correlative units in the region. Similarities between the McKellar Harbour Formation and sedimentary rocks composing the fore-arc basin and Quetico trench to the north indicate that by 2696 Ma the trench had been overwhelmed by sediment, to the point where turbidity currents were overflowing onto the abyssal ocean plain, building a prograding submarine ramp–fan that was to become the McKellar Harbour Formation. The turbiditic ramp–fan assemblage comprising most of this extensive depositional system crosses much of southern Superior Province, highlighting the interrelated genesis of rocks formed during amalgamation of the individual subprovinces. \u003C\u002Fjats:p>",{"EN":1795},"Neoarchean trans-subprovince sediment transport in southwestern Superior Province: sedimentological, geochemical, and geochronological evidence",{"VOID":1797},"10.1139\u002Fe06-059",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe06-059",[1801,1820,1835],{"id":1802,"sortIndex":25,"researcher":24,"roles":1803,"affiliations":1804,"properties":1813,"displayName":1817,"givenName":24,"familyName":24},"53e6bd98-c416-42a6-aa2b-930649d569ba",[],[1805],{"id":1806,"sortIndex":25,"affiliation":1807,"properties":24},"0f501c98-f9fb-404b-bcae-f712f69b80f4",{"id":1806,"createTime":24,"updateTime":24,"relativeEntities":1808,"slug":24,"properties":1809,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1812,"statistic":24},[],{"title":1810},{"VI":1811},"Department of Geology, Lakehead University, Thunder Bay, ON P7B 5E1, Canada",[],{"orcid":1814,"title":1816,"openalex":1818},{"VOID":1815},"https:\u002F\u002Forcid.org\u002F0000-0001-6188-6288",{"EN":1817},"Philip Fralick",{"VOID":1819},"A5045064202",{"id":1821,"sortIndex":125,"researcher":24,"roles":1822,"affiliations":1823,"properties":1830,"displayName":1832,"givenName":24,"familyName":24},"c94644d3-5ca1-434c-b2dc-8f5f23da2100",[],[1824],{"id":1806,"sortIndex":25,"affiliation":1825,"properties":24},{"id":1806,"createTime":24,"updateTime":24,"relativeEntities":1826,"slug":24,"properties":1827,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1829,"statistic":24},[],{"title":1828},{"VI":1811},[],{"title":1831,"openalex":1833},{"EN":1832},"R H Purdon",{"VOID":1834},"A5019950605",{"id":1836,"sortIndex":262,"researcher":24,"roles":1837,"affiliations":1838,"properties":1847,"displayName":1851,"givenName":24,"familyName":24},"9c0695c7-0236-4263-bda3-f59bf3ef3587",[],[1839],{"id":1840,"sortIndex":25,"affiliation":1841,"properties":24},"3fb0f7ed-2f72-461d-87cc-c456c28389f6",{"id":1840,"createTime":24,"updateTime":24,"relativeEntities":1842,"slug":24,"properties":1843,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1846,"statistic":24},[],{"title":1844},{"VI":1845},"Department of Geology, University of Toronto, Toronto, ON M5S 3B1, Canada",[],{"orcid":1848,"title":1850,"openalex":1852},{"VOID":1849},"https:\u002F\u002Forcid.org\u002F0000-0003-2579-7442",{"EN":1851},"Donald W. Davis",{"VOID":1853},"A5054079799",{"url":24,"publisher":1855,"properties":1893},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1856,"slug":10,"properties":1857,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1862,"manageAffiliations":1867,"indexDatabases":1878,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1858,"eissn":1859,"issn":1860,"title":1861},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[1863],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":1864,"label":1865,"description":1866,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[1868,1873],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":1869,"slug":24,"properties":1870,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1872,"statistic":24},[],{"title":1871},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":1874,"slug":24,"properties":1875,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1877,"statistic":24},[],{"title":1876},{"EN":46},[],[1879,1886],{"id":67,"indexDatabase":1880,"url":78,"indexYears":79,"academicFieldIds":1885,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":1881,"label":1882,"description":1883,"key":75,"publicationTags":1884,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"id":50,"indexDatabase":1887,"url":63,"indexYears":24,"academicFieldIds":1892,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":1888,"label":1889,"description":1890,"key":59,"publicationTags":1891,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"issue":1894,"pages":1895,"volume":1897},{"VOID":966},{"VOID":1896},"1055-1070",{"VOID":970},23,{"total":1898,"publishYear":973,"statisticByYear":1900},{"2012":282,"2013":262,"2015":125,"2017":125,"2018":125,"2020":125,"2021":125,"2022":282,"2023":125,"2024":125},[61,82],[1903,1907,1909,1912,1915,1918,1921,1923,1926,1928,1930,1934,1937,1940,1944,1948,1952,1955,1959,1963,1965,1968,1970,1973,1976,1980,1983,1987],{"id":24,"text":1904,"url":24,"identifiers":1905},"Barrett T.J., 1989, Sedimentology, 36, 221, 10.1111\u002Fj.1365-3091.1989.tb00604.x",{"doi":1906},"10.1111\u002Fj.1365-3091.1989.tb00604.x",{"id":24,"text":1062,"url":24,"identifiers":1908},{},{"id":24,"text":1910,"url":24,"identifiers":1911},"Corfu F., 1989, Chemical Geology, 79, 183",{},{"id":24,"text":1913,"url":24,"identifiers":1914},"Corfu F., 1998, Bulletin of the Geological Society of America, 110, 1467, 10.1130\u002F0016-7606(1998)110\u003C1467:SGBWSP>2.3.CO;2",{"doi":1121},{"id":24,"text":1916,"url":24,"identifiers":1917},"Davis D.W., 1995, Lithoprobe Report, 53, 18",{},{"id":24,"text":1919,"url":24,"identifiers":1920},"Davis D.W., 1998, Lithoprobe Report, 65, 21",{},{"id":24,"text":1143,"url":24,"identifiers":1922},{"doi":1145},{"id":24,"text":1924,"url":24,"identifiers":1925},"Davis D.W., 2003, Economic Geology, 98, 51",{},{"id":24,"text":1178,"url":24,"identifiers":1927},{"doi":1180},{"id":24,"text":1189,"url":24,"identifiers":1929},{"doi":1191},{"id":24,"text":1931,"url":24,"identifiers":1932},"Eriksson K.A., 1994, Earth Science Reviews, 37, 1, 10.1016\u002F0012-8252(94)90025-6",{"doi":1933},"10.1016\u002F0012-8252(94)90025-6",{"id":24,"text":1935,"url":24,"identifiers":1936},"Fralick P.W., 2003, Geotext, 4, 85",{},{"id":24,"text":1938,"url":24,"identifiers":1939},"Fralick P.W., 1995, Special Publication, 22, 137",{},{"id":24,"text":1941,"url":24,"identifiers":1942},"Fralick P.W., 1997, Sedimentary Geology, 113, 111, 10.1016\u002FS0037-0738(97)00049-3",{"doi":1943},"10.1016\u002FS0037-0738(97)00049-3",{"id":24,"text":1945,"url":24,"identifiers":1946},"Fralick P.W., 1992, Canadian Shield. Canadian Journal of Earth Sciences, 29, 2551, 10.1139\u002Fe92-202",{"doi":1947},"10.1139\u002Fe92-202",{"id":24,"text":1949,"url":24,"identifiers":1950},"Ghibaudo G., 1992, Sedimentology, 39, 423, 10.1111\u002Fj.1365-3091.1992.tb02126.x",{"doi":1951},"10.1111\u002Fj.1365-3091.1992.tb02126.x",{"id":24,"text":1953,"url":24,"identifiers":1954},"Jaffey A.H., 1971, Physical Review, 4, 1889",{},{"id":24,"text":1956,"url":24,"identifiers":1957},"Krogh T.E., 1973, Geochimica et Cosmochimica Acta, 37, 485, 10.1016\u002F0016-7037(73)90213-5",{"doi":1958},"10.1016\u002F0016-7037(73)90213-5",{"id":24,"text":1960,"url":24,"identifiers":1961},"Krogh T.E., 1982, Geochimica et Cosmochimica Acta, 46, 637, 10.1016\u002F0016-7037(82)90165-X",{"doi":1962},"10.1016\u002F0016-7037(82)90165-X",{"id":24,"text":1346,"url":24,"identifiers":1964},{"doi":1348},{"id":24,"text":1966,"url":24,"identifiers":1967},"Percival J.A., 1989, Canadian Journal of Earth Sciences, 23, 158",{},{"id":24,"text":1426,"url":24,"identifiers":1969},{"doi":1428},{"id":24,"text":1971,"url":24,"identifiers":1972},"Stockwell C.H., 1964, Paper, 64, 1",{},{"id":24,"text":1974,"url":24,"identifiers":1975},"Walker R.G., 1978, American Association of Petroleum Geologists Bulletin, 62, 932",{},{"id":24,"text":1977,"url":24,"identifiers":1978},"Williams H.R., 1990, Canadian Journal of Earth Science, 27, 570, 10.1139\u002Fe90-053",{"doi":1979},"10.1139\u002Fe90-053",{"id":24,"text":1981,"url":24,"identifiers":1982},"Wilson J.T., 1949, Royal Society of Canada Transactions, 43",{},{"id":24,"text":1984,"url":24,"identifiers":1985},"Winchester J.A., 1977, Chemical Geology, 20, 325, 10.1016\u002F0009-2541(77)90057-2",{"doi":1986},"10.1016\u002F0009-2541(77)90057-2",{"id":24,"text":1685,"url":24,"identifiers":1988},{"doi":1687},{"id":1990,"createTime":1991,"updateTime":1991,"relativeEntities":1992,"slug":1993,"properties":1994,"entityType":106,"verifyStatus":217,"verifyTime":1991,"verifyNote":218,"languages":2005,"translateLanguages":24,"viewCount":25,"primaryUrl":2006,"fullTextUrl":24,"authors":2007,"publicationType":133,"publisherRelationship":2025,"citationCount":356,"citationInfo":2071,"publishDate":2074,"publishYear":2072,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2075,"openAccess":24,"references":2076,"isForceReanalyzing":200},"0fe8466c-07f5-4cb3-bc4d-0a06fb590f97","2024-12-12T13:48:57.324+00:00",[],"Structural-evolution-of-the-Hemlo-greenstone-belt-in-the-vicinity-of-the-world-class-Hemlo-gold-deposit",{"openalex":1995,"mag":1997,"abstract":1999,"title":2001,"doi":2003},{"VOID":1996},"W2080089730",{"VOID":1998},"2080089730",{"EN":2000},"\u003Cjats:p> A complex history of volcano-sedimentary deposition, polyphase strain, multiple intrusive events, and various stages of porphyroblastesis is indicated for the Hemlo gold deposit area within the Hemlo greenstone belt. Structural elements can be assigned to at least six stages of development (D\u003Cjats:sub>1\u003C\u002Fjats:sub>–D\u003Cjats:sub>6\u003C\u002Fjats:sub>). D\u003Cjats:sub>1\u003C\u002Fjats:sub> generated small-scale folds and low-angle faults (thrusts?) with no planar fabric, except within strain aureoles around the earliest intrusions. D\u003Cjats:sub>2\u003C\u002Fjats:sub> was a progressive event resulting from northeast-directed compression, which generated regional, predominantly S-shaped folds (early D\u003Cjats:sub>2\u003C\u002Fjats:sub>); penetrative planar and linear fabrics, overturned stratigraphy, and formation of an inflection in the strike of the greenstone belt (mid-D\u003Cjats:sub>2\u003C\u002Fjats:sub>); and development of high-strain zones with dominant sinistral and local dextral shear sense (late D\u003Cjats:sub>2\u003C\u002Fjats:sub>). D\u003Cjats:sub>3\u003C\u002Fjats:sub> was a distinctly separate progressive event resulting from northwest-directed transpression, which generated variably penetrative east- to northeast-striking foliation (S\u003Cjats:sub>3\u003C\u002Fjats:sub>), ductile dextral shear fabrics, and small-scale Z-shaped folds (early D\u003Cjats:sub>3\u003C\u002Fjats:sub>), followed by brittle–ductile to brittle development of cataclasite and pseudotachylite in layer-parallel zones (late D\u003Cjats:sub>3\u003C\u002Fjats:sub>). D\u003Cjats:sub>4\u003C\u002Fjats:sub> resulted in contractional kinks and brittle fractures, locally in conjugate sets. D\u003Cjats:sub>5\u003C\u002Fjats:sub> and D\u003Cjats:sub>6\u003C\u002Fjats:sub> are represented by brittle to brittle–ductile faults, which overprint Paleoproterozoic and Mesoproterozoic dikes, respectively. Four granitoid magmatic events span the interval 2720–2677 Ma, with emplacement mainly during D\u003Cjats:sub>2\u003C\u002Fjats:sub>, between ca. 2690 and ca. 2684 Ma. A protracted period of regional medium-grade metamorphism likely spanned the D\u003Cjats:sub>2\u003C\u002Fjats:sub>–D\u003Cjats:sub>3\u003C\u002Fjats:sub> stages. The Hemlo gold deposit was emplaced during mid-D\u003Cjats:sub>2\u003C\u002Fjats:sub> and was largely controlled by D\u003Cjats:sub>2\u003C\u002Fjats:sub> structural elements and competency contrast between rock units. \u003C\u002Fjats:p>",{"EN":2002},"Structural evolution of the Hemlo greenstone belt in the vicinity of the world-class Hemlo gold deposit",{"VOID":2004},"10.1139\u002Fe03-004",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe03-004",[2008],{"id":2009,"sortIndex":25,"researcher":24,"roles":2010,"affiliations":2011,"properties":2020,"displayName":2022,"givenName":24,"familyName":24},"c49851f3-52fe-42dd-b64d-b645b1f903a5",[],[2012],{"id":2013,"sortIndex":25,"affiliation":2014,"properties":24},"f3bacc9e-52c9-4b12-bf4e-8b757bcc52d9",{"id":2013,"createTime":24,"updateTime":24,"relativeEntities":2015,"slug":24,"properties":2016,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2019,"statistic":24},[],{"title":2017},{"EN":2018},"Precambrian Geology Section, Ontario Geological Survey, 933 Ramsey Lake Road, Sudbury, ON P3E 6B5, Canada (e-mail: ).",[],{"title":2021,"openalex":2023},{"EN":2022},"T.L. 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Z.G., 1990, Miscellaneous Paper, 150, 107",{},{"id":24,"text":2081,"url":24,"identifiers":2082},"Ayer J., 2002, Precambrian Research, 115, 63, 10.1016\u002FS0301-9268(02)00006-2",{"doi":2083},"10.1016\u002FS0301-9268(02)00006-2",{"id":24,"text":2085,"url":24,"identifiers":2086},"Bauer R.L., 1992, Canadian Journal of Earth Sciences, 29, 2087, 10.1139\u002Fe92-166",{"doi":2087},"10.1139\u002Fe92-166",{"id":24,"text":2089,"url":24,"identifiers":2090},"Beakhouse G.P., 1998, Open File Report, 5977, 1",{},{"id":24,"text":2092,"url":24,"identifiers":2093},"Behrendt J.C., 1988, Geology, 16, 81, 10.1130\u002F0091-7613(1988)016\u003C0081:CSOTMR>2.3.CO;2",{"doi":2094},"10.1130\u002F0091-7613(1988)016\u003C0081:CSOTMR>2.3.CO;2",{"id":24,"text":2096,"url":24,"identifiers":2097},"Bodycomb V., 2000, Extended Abstracts, 25, 1094",{},{"id":24,"text":2099,"url":24,"identifiers":2100},"Buchan K.L., 1993, Canadian Journal of Earth Sciences, 30, 1286, 10.1139\u002Fe93-110",{"doi":2101},"10.1139\u002Fe93-110",{"id":24,"text":2103,"url":24,"identifiers":2104},"Buchan K.L., 1996, Canadian Journal of Earth Sciences, 33, 1583, 10.1139\u002Fe96-120",{"doi":2105},"10.1139\u002Fe96-120",{"id":24,"text":2107,"url":24,"identifiers":2108},"Cameron E.M., 1985, Geochimica et Cosmochimica Acta, 49, 2041, 10.1016\u002F0016-7037(85)90062-6",{"doi":2109},"10.1016\u002F0016-7037(85)90062-6",{"id":24,"text":1910,"url":24,"identifiers":2111},{},{"id":24,"text":2113,"url":24,"identifiers":2114},"Corfu F., 1989, Chemical Geology, 79, 201",{},{"id":24,"text":1119,"url":24,"identifiers":2116},{"doi":1121},{"id":24,"text":2118,"url":24,"identifiers":2119},"Davis D.W., 1998, Ont., 5, 1",{},{"id":24,"text":2121,"url":24,"identifiers":2122},"Davis D.W., 1998, Open File Report, 5977, 1",{},{"id":24,"text":2124,"url":24,"identifiers":2125},"Easton R.M., 2000, The Canadian Mineralogist, 38, 287, 10.2113\u002Fgscanmin.38.2.287",{"doi":2126},"10.2113\u002Fgscanmin.38.2.287",{"id":24,"text":2128,"url":24,"identifiers":2129},"Grasemann B., 2001, Journal of Structural Geology, 23, 715, 10.1016\u002FS0191-8141(00)00108-5",{"doi":2130},"10.1016\u002FS0191-8141(00)00108-5",{"id":24,"text":2132,"url":24,"identifiers":2133},"Hagemann S.G., 2000, Reviews in Economic Geology, 13, 9",{},{"id":24,"text":2135,"url":24,"identifiers":2136},"Hugon H., 1984, Miscellaneous Paper, 119, 212",{},{"id":24,"text":2138,"url":24,"identifiers":2139},"Jackson S.L., 1998, Open File Report, 5977, 1",{},{"id":24,"text":2141,"url":24,"identifiers":2142},"Jackson S.L., 1991, Special, 4, 405",{},{"id":24,"text":2144,"url":24,"identifiers":2145},"Jirsa M.A., 1992, Canadian Journal of Earth Sciences, 29, 2146, 10.1139\u002Fe92-170",{"doi":2146},"10.1139\u002Fe92-170",{"id":24,"text":2148,"url":24,"identifiers":2149},"Knight J.T., 1993, Mineralium Deposita, 28, 436, 10.1007\u002FBF02431601",{"doi":2150},"10.1007\u002FBF02431601",{"id":24,"text":2152,"url":24,"identifiers":2153},"Kretz R., 1983, American Mineralogist, 68, 277",{},{"id":24,"text":2155,"url":24,"identifiers":2156},"Kuhns R.J., 1994, Economic Geology, 89, 720, 10.2113\u002Fgsecongeo.89.4.720",{"doi":2157},"10.2113\u002Fgsecongeo.89.4.720",{"id":24,"text":2159,"url":24,"identifiers":2160},"Lin S., 2001, Economic Geology, 96, 477, 10.2113\u002Fgsecongeo.96.3.477",{"doi":2161},"10.2113\u002Fgsecongeo.96.3.477",{"id":24,"text":2163,"url":24,"identifiers":2164},"Masliwec A., 1986, Miscellaneous Paper, 130, 107",{},{"id":24,"text":2166,"url":24,"identifiers":2167},"McGill G.E., 1992, Canadian Journal of Earth Sciences, 29, 2118, 10.1139\u002Fe92-168",{"doi":2168},"10.1139\u002Fe92-168",{"id":24,"text":2170,"url":24,"identifiers":2171},"Michibayashi K., 1991, University of Western Australia Publication, 25, 90",{},{"id":24,"text":2173,"url":24,"identifiers":2174},"Michibayashi K., 1995, Ore Geology Reviews, 10, 31, 10.1016\u002F0169-1368(95)00004-L",{"doi":2175},"10.1016\u002F0169-1368(95)00004-L",{"id":24,"text":2177,"url":24,"identifiers":2178},"Muir T.L., 1986, Miscellaneous Paper, 132, 95",{},{"id":24,"text":2180,"url":24,"identifiers":2181},"Muir T.L., 1995, Ontario Geological Survey, Map 2629, Scale, 1, 20",{},{"id":24,"text":2183,"url":24,"identifiers":2184},"Muir T.L., 2000, Ontario Geological Survey, Map 2614, Scale, 1, 50",{},{"id":24,"text":2186,"url":24,"identifiers":2187},"Muir T.L., 2002, Ore Geology Reviews, 21, 1, 10.1016\u002FS0169-1368(02)00066-5",{"doi":2188},"10.1016\u002FS0169-1368(02)00066-5",{"id":24,"text":2190,"url":24,"identifiers":2191},"Muir T.L., 1987, Miscellaneous Paper, 137, 117",{},{"id":24,"text":2193,"url":24,"identifiers":2194},"Osmani I.A., 1991, Special, 4, 661",{},{"id":24,"text":2196,"url":24,"identifiers":2197},"Pan Y., 1992, Economic Geology, 87, 1104, 10.2113\u002Fgsecongeo.87.4.1104",{"doi":2198},"10.2113\u002Fgsecongeo.87.4.1104",{"id":24,"text":2200,"url":24,"identifiers":2201},"Pan Y., 1993, Canadian Journal of Earth Sciences, 30, 985, 10.1139\u002Fe93-082",{"doi":2202},"10.1139\u002Fe93-082",{"id":24,"text":2204,"url":24,"identifiers":2205},"Pan Y., 1995, Ore Geology Reviews, 9, 455, 10.1016\u002F0169-1368(95)00003-K",{"doi":2206},"10.1016\u002F0169-1368(95)00003-K",{"id":24,"text":2208,"url":24,"identifiers":2209},"Pan Y., 1991, Precambrian Research, 52, 53, 10.1016\u002F0301-9268(91)90013-Z",{"doi":2210},"10.1016\u002F0301-9268(91)90013-Z",{"id":24,"text":2212,"url":24,"identifiers":2213},"Pan Y., 1991, Economic Geology, 86, 1626, 10.2113\u002Fgsecongeo.86.8.1626",{"doi":2214},"10.2113\u002Fgsecongeo.86.8.1626",{"id":24,"text":2216,"url":24,"identifiers":2217},"Parker J.R., 2000, Open File Report, 6032, 22",{},{"id":24,"text":2219,"url":24,"identifiers":2220},"Passchier C.W., 2001, Journal of Structural Geology, 23, 951, 10.1016\u002FS0191-8141(00)00166-8",{"doi":2221},"10.1016\u002FS0191-8141(00)00166-8",{"id":24,"text":2223,"url":24,"identifiers":2224},"Peterson V.L., 1999, Canadian Journal of Earth Sciences, 36, 605, 10.1139\u002Fe99-013",{"doi":2225},"10.1139\u002Fe99-013",{"id":24,"text":2227,"url":24,"identifiers":2228},"Powell W.G., 1999, Canadian Journal of Earth Sciences, 36, 33, 10.1139\u002Fe98-078",{"doi":2229},"10.1139\u002Fe98-078",{"id":24,"text":2231,"url":24,"identifiers":2232},"Queen M., 1996, Canadian Journal of Earth Sciences, 33, 958, 10.1139\u002Fe96-072",{"doi":2233},"10.1139\u002Fe96-072",{"id":24,"text":2235,"url":24,"identifiers":2236},"Robert F., 1997, Australian Journal of Earth Sciences, 44, 329, 10.1080\u002F08120099708728316",{"doi":2237},"10.1080\u002F08120099708728316",{"id":24,"text":2239,"url":24,"identifiers":2240},"Robert F., 2001, Richards and R.M. Tosdal. Reviews in Economic Geology, 14, 111",{},{"id":24,"text":2242,"url":24,"identifiers":2243},"Schmid R., 1981, Geology, 9, 41, 10.1130\u002F0091-7613(1981)9\u003C41:DNACOP>2.0.CO;2",{"doi":2244},"10.1130\u002F0091-7613(1981)9\u003C41:DNACOP>2.0.CO;2",{"id":24,"text":2246,"url":24,"identifiers":2247},"Stein H.J., 2000, Abstracts with Programs, 32, A424",{},{"id":24,"text":2249,"url":24,"identifiers":2250},"Tabor J.R., 1991, Canadian Journal of Earth Sciences, 28, 292, 10.1139\u002Fe91-028",{"doi":2251},"10.1139\u002Fe91-028",{"id":24,"text":2253,"url":24,"identifiers":2254},"Williams H.R., 1991, Special, 4, 485",{},{"id":24,"text":2256,"url":24,"identifiers":2257},"Wyman D.A., 1989, Journal of Geophysical Research, 94, 4667, 10.1029\u002FJB094iB04p04667",{"doi":2258},"10.1029\u002FJB094iB04p04667",{"id":24,"text":1685,"url":24,"identifiers":2260},{"doi":1687},{"id":2262,"createTime":2263,"updateTime":2263,"relativeEntities":2264,"slug":2265,"properties":2266,"entityType":106,"verifyStatus":217,"verifyTime":2277,"verifyNote":218,"languages":2278,"translateLanguages":24,"viewCount":25,"primaryUrl":2279,"fullTextUrl":24,"authors":2280,"publicationType":133,"publisherRelationship":2327,"citationCount":2372,"citationInfo":2373,"publishDate":2377,"publishYear":2374,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2378,"openAccess":24,"references":2379,"isForceReanalyzing":200},"2c8dd1a7-b6ae-4eaf-84f9-88acad851503","2024-12-12T13:48:49.194+00:00",[],"The-age-of-the-Gunflint-Formation-Ontario-Canada-single-zircon-U-Pb-age-determinations-from-reworked-volcanic-ash",{"openalex":2267,"mag":2269,"abstract":2271,"title":2273,"doi":2275},{"VOID":2268},"W2037568805",{"VOID":2270},"2037568805",{"EN":2272},"\u003Cjats:p> The Gunflint Formation, a Paleoproterozoic chemical–clastic sedimentary assemblage outcropping to the immediate northwest of Lake Superior, became famous in 1954 as containing the oldest fossil assemblage known at that time. Older microfossils have since been discovered, but the Gunflint procaryotes remain one of the most diverse Precambrian fossil communities. The finding of possible multicellular organisms in correlative lithic units in Michigan has recently added to the need for an exact age of the Formation. Zircons were extracted from rainout and storm reworked volcanoclastic beds in the upper portion of the Gunflint Formation. A euhedral zircon population has yielded a 1878.3 ± 1.3 million years BP U–Pb age, believed to be nearly synchronous with the depositional age. This not only provides a precise age for the community of organisms, but also strongly supports a back-arc extensional setting for the Animikie Basin, rather than a foreland trough. \u003C\u002Fjats:p>",{"EN":2274},"The age of the Gunflint Formation, Ontario, Canada: single zircon U–Pb age determinations from reworked volcanic ash",{"VOID":2276},"10.1139\u002Fe02-028","2024-12-12T13:48:49.193+00:00",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe02-028",[2281,2295,2312],{"id":2282,"sortIndex":25,"researcher":24,"roles":2283,"affiliations":2284,"properties":2291,"displayName":1817,"givenName":24,"familyName":24},"72e4fc3a-8a70-4cd6-8c02-0c431ac42d81",[],[2285],{"id":1806,"sortIndex":25,"affiliation":2286,"properties":24},{"id":1806,"createTime":24,"updateTime":24,"relativeEntities":2287,"slug":24,"properties":2288,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2290,"statistic":24},[],{"title":2289},{"VI":1811},[],{"orcid":2292,"title":2293,"openalex":2294},{"VOID":1815},{"EN":1817},{"VOID":1819},{"id":2296,"sortIndex":125,"researcher":24,"roles":2297,"affiliations":2298,"properties":2307,"displayName":2309,"givenName":24,"familyName":24},"e667c421-8712-498d-9a30-cdccfe50929f",[],[2299],{"id":2300,"sortIndex":25,"affiliation":2301,"properties":24},"d96d90f2-3590-49da-908b-6758487cfbfc",{"id":2300,"createTime":24,"updateTime":24,"relativeEntities":2302,"slug":24,"properties":2303,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2306,"statistic":24},[],{"title":2304},{"EN":2305},"Earth Sciences Department, Royal Ontario Museum, 100 Queen’s Park, Toronto, ON M5S 2C6, Canada.",[],{"title":2308,"openalex":2310},{"EN":2309},"D. W. Davis",{"VOID":2311},"A5090501193",{"id":2313,"sortIndex":262,"researcher":24,"roles":2314,"affiliations":2315,"properties":2322,"displayName":2324,"givenName":24,"familyName":24},"dd4883b1-a9f5-40ef-8d36-3e80eb2bc74c",[],[2316],{"id":1806,"sortIndex":25,"affiliation":2317,"properties":24},{"id":1806,"createTime":24,"updateTime":24,"relativeEntities":2318,"slug":24,"properties":2319,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2321,"statistic":24},[],{"title":2320},{"VI":1811},[],{"title":2323,"openalex":2325},{"EN":2324},"S. A. 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K.M., 1989, Geological Society of America Bulletin, 101, 333, 10.1130\u002F0016-7606(1989)101\u003C0333:NIATOO>2.3.CO;2",{"doi":2383},"10.1130\u002F0016-7606(1989)101\u003C0333:NIATOO>2.3.CO;2",{"id":24,"text":2385,"url":24,"identifiers":2386},"Bell R., 1870, Report for, 1866, 313",{},{"id":24,"text":2388,"url":24,"identifiers":2389},"Davis D.W., 1982, Canadian Journal of Earth Sciences, 19, 2141, 10.1139\u002Fe82-188",{"doi":2390},"10.1139\u002Fe82-188",{"id":24,"text":2392,"url":24,"identifiers":2393},"Edhorn A-S, 1973, Proceedings of the Geological Association of Canada, 25, 37",{},{"id":24,"text":2395,"url":24,"identifiers":2396},"Faure G., 1969, Geological Society of America Bulletin, 80, 1725, 10.1130\u002F0016-7606(1969)80[1725:TAOTGI]2.0.CO;2",{"doi":2397},"10.1130\u002F0016-7606(1969)80[1725:TAOTGI]2.0.CO;2",{"id":24,"text":2399,"url":24,"identifiers":2400},"Fralick P.W., 1995, Special Publication, 137",{},{"id":24,"text":2402,"url":24,"identifiers":2403},"Franklin J.M., 1978, Report 2, Geological Survey of Canada, Paper, 77, 35",{},{"id":24,"text":2405,"url":24,"identifiers":2406},"Gerlach D.C., 1988, EOS, 69, 1515",{},{"id":24,"text":2408,"url":24,"identifiers":2409},"Grout F.F., 1919, American Journal of Science, 48, 199, 10.2475\u002Fajs.s4-48.285.199",{"doi":2410},"10.2475\u002Fajs.s4-48.285.199",{"id":24,"text":2412,"url":24,"identifiers":2413},"Hassler S.W., 1989, Canadian Journal of Earth Sciences, 26, 1574, 10.1139\u002Fe89-134",{"doi":2414},"10.1139\u002Fe89-134",{"id":24,"text":2416,"url":24,"identifiers":2417},"Hemming S.R., 1990, EOS, 71, 654",{},{"id":24,"text":2419,"url":24,"identifiers":2420},"Hemming S.R., 1995, The Journal of Geology, 103, 147, 10.1086\u002F629733",{"doi":2421},"10.1086\u002F629733",{"id":24,"text":2423,"url":24,"identifiers":2424},"Hoffman P.F., 1987, Geodynamics Series, 17, 85, 10.1029\u002FGD017p0085",{"doi":2425},"10.1029\u002FGD017p0085",{"id":24,"text":2427,"url":24,"identifiers":2428},"Hurley P.M., 1962, Journal of Geology, 70, 489, 10.1086\u002F626839",{"doi":2429},"10.1086\u002F626839",{"id":24,"text":1953,"url":24,"identifiers":2431},{},{"id":24,"text":2433,"url":24,"identifiers":2434},"Kissin S.A., 1994, Proceedings of the Institute on Lake Superior Geology, 40, 18",{},{"id":24,"text":1956,"url":24,"identifiers":2436},{"doi":1958},{"id":24,"text":1960,"url":24,"identifiers":2438},{"doi":1962},{"id":24,"text":2440,"url":24,"identifiers":2441},"Moorhouse W.W., 1962, Royal Society of Canada Transactions, 56, 97",{},{"id":24,"text":2443,"url":24,"identifiers":2444},"Morey G.B., 1995, Economic Geology, 90, 1983, 10.2113\u002Fgsecongeo.90.7.1983",{"doi":2445},"10.2113\u002Fgsecongeo.90.7.1983",{"id":24,"text":2447,"url":24,"identifiers":2448},"Peterman Z.E., 1966, Geological Society of America Bulletin, 77, 1031, 10.1130\u002F0016-7606(1966)77[1031:RDOMPM]2.0.CO;2",{"doi":2449},"10.1130\u002F0016-7606(1966)77[1031:RDOMPM]2.0.CO;2",{"id":24,"text":2451,"url":24,"identifiers":2452},"Pufahl P.K., 1995, In Proceedings of the Institute of Lake Superior Geology, 41, 59",{},{"id":24,"text":2454,"url":24,"identifiers":2455},"Sims P.K., 1985, Geological Society of America Bulletin, 96, 1101, 10.1130\u002F0016-7606(1985)96\u003C1101:TDGDIF>2.0.CO;2",{"doi":2456},"10.1130\u002F0016-7606(1985)96\u003C1101:TDGDIF>2.0.CO;2",{"id":24,"text":2458,"url":24,"identifiers":2459},"Sims P.K., 1989, Canadian Journal of Earth Sciences, 26, 2145, 10.1139\u002Fe89-180",{"doi":2460},"10.1139\u002Fe89-180",{"id":24,"text":2462,"url":24,"identifiers":2463},"Stille P., 1986, Geochemica et Cosmochimica Acta, 50, 1141, 10.1016\u002F0016-7037(86)90395-9",{"doi":2464},"10.1016\u002F0016-7037(86)90395-9",{"id":24,"text":2466,"url":24,"identifiers":2467},"Ueng W.C., 1988, Canadian Journal of Earth Sciences, 25, 528, 10.1139\u002Fe88-052",{"doi":2468},"10.1139\u002Fe88-052",{"id":2470,"createTime":2471,"updateTime":2471,"relativeEntities":2472,"slug":2473,"properties":2474,"entityType":106,"verifyStatus":23,"verifyTime":2485,"verifyNote":107,"languages":2486,"translateLanguages":24,"viewCount":25,"primaryUrl":2487,"fullTextUrl":24,"authors":2488,"publicationType":133,"publisherRelationship":2506,"citationCount":2550,"citationInfo":2551,"publishDate":2553,"publishYear":1777,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2554,"openAccess":24,"references":2555,"isForceReanalyzing":200},"231a4ef0-c249-4589-a903-73036306feeb","2024-12-12T13:48:45.670+00:00",[],"Oxygen-Isotope-Geochemistry-of-Submarine-Greenstones",{"openalex":2475,"mag":2477,"abstract":2479,"title":2481,"doi":2483},{"VOID":2476},"W2006949523",{"VOID":2478},"2006949523",{"EN":2480},"\u003Cjats:p> Most submarine greenstones recovered from the North Mid-Atlantic Ridge range in δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O from 2.8 to 6.8‰ (SMOW). An extremely light rock. (δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O = −7.1‰), was also analyzed, but it might be an ice rafted erratic. The heavier ones, up to 8‰, are probably weathered. On the average, the δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O of 14 greenstones is slightly lower than that of fresh unmetamorphosed submarine basalt. The \u003Cjats:sup>18\u003C\u002Fjats:sup>O fractionations between coexisting metamorphic minerals of the greenstones are consistent with the independently inferred range of metamorphic temperatures of 200–300 °C. The δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O of the possible metamorphic water can be estimated from this temperature range and the δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O of the metamorphic minerals to be − 2 to + 2‰. This argues strongly that little or no 'juvenile' water (water outgassed from the mantle) participated directly in the metamorphism. The δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O data are consistent with the participation of sea water in the metamorphism. Similar conclusions can be drawn from the \u003Cjats:sup>18\u003C\u002Fjats:sup>O analyses of a submarine diabase and two gabbros. Disseminated carbonates in the greenstones have δ\u003Cjats:sup>18\u003C\u002Fjats:sup>C values typically found in carbonatites or partially decarbonated marine limestones. \u003C\u002Fjats:p>",{"EN":2482},"Oxygen Isotope Geochemistry of Submarine Greenstones",{"VOID":2484},"10.1139\u002Fe72-038","2024-12-12T13:48:45.669+00:00",[109],"http:\u002F\u002Fwww.nrcresearchpress.com\u002Fdoi\u002F10.1139\u002Fe72-038",[2489,2499],{"id":2490,"sortIndex":25,"researcher":24,"roles":2491,"affiliations":2492,"properties":2493,"displayName":1718,"givenName":24,"familyName":24},"3d79a118-c720-47a5-80ae-51af386ee055",[],[],{"orcid":2494,"title":2496,"openalex":2497},{"VOID":2495},"https:\u002F\u002Forcid.org\u002F0000-0003-2768-2972",{"EN":1718},{"VOID":2498},"A5003741365",{"id":2500,"sortIndex":125,"researcher":24,"roles":2501,"affiliations":2502,"properties":2503,"displayName":1727,"givenName":24,"familyName":24},"54a72a74-f3fb-42e6-a48c-cfbc78e9afbc",[],[],{"title":2504,"openalex":2505},{"EN":1727},{"VOID":1729},{"url":24,"publisher":2507,"properties":2545},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":2508,"slug":10,"properties":2509,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":2514,"manageAffiliations":2519,"indexDatabases":2530,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":2510,"eissn":2511,"issn":2512,"title":2513},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[2515],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":2516,"label":2517,"description":2518,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[2520,2525],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":2521,"slug":24,"properties":2522,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2524,"statistic":24},[],{"title":2523},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":2526,"slug":24,"properties":2527,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2529,"statistic":24},[],{"title":2528},{"EN":46},[],[2531,2538],{"id":67,"indexDatabase":2532,"url":78,"indexYears":79,"academicFieldIds":2537,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":2533,"label":2534,"description":2535,"key":75,"publicationTags":2536,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"id":50,"indexDatabase":2539,"url":63,"indexYears":24,"academicFieldIds":2544,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":2540,"label":2541,"description":2542,"key":59,"publicationTags":2543,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"issue":2546,"pages":2547,"volume":2549},{"VOID":175},{"VOID":2548},"471-478",{"VOID":1774},164,{"total":2550,"publishYear":1777,"statisticByYear":2552},{"2012":282,"2013":282,"2014":262,"2015":350,"2017":125,"2018":282,"2019":125,"2020":262,"2021":262,"2022":892,"2023":282,"2024":125},"1972-05-01",[61],[]]