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The journal prides itself on the quality of its graphics and photographic reproduction. The Editors are keen to encourage interdisciplinary papers and Transactions also publishes occasional special symposia and invited volumes of specific interest. 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The blocks show degrees of melting from 0–50 vol%. Because very few have adhering juvenile magma, it is thought that the blocks are fragments of the Holocene magma chamber's walls. Primary crystallisation of granodiorite produced phenocrystic pl + hyp + aug + mt + il + ap + zc, followed by qz + hb + bt + alkali feldspar (af). Presence of fluid inclusions in all samples implies complete crystallisation before melting. Subsolidus exchange with meteoric hydrothermal fluids before melting is evident in δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O values of −3·4+4·9‰ for quartz and plagioclase in partially melted granodiorites (fresh lavas from the region have δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O values of +5·8−+7·0‰); δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O values of unmelted granodiorites from preclimatic eruptive units suggest hydrothermal exchange began between ∼70 and 24 ka. Before eruption, the granitic rocks equilibrated at temperatures, estimated from Fe-Ti oxide compositions, of up to ∼1000°C for c. 10\u003Cjats:sup>2\u003C\u002Fjats:sup>–10\u003Cjats:sup>4\u003C\u002Fjats:sup> years at a minimum pressure of 100-180 MPa. Heating caused progressive breakdown or dissolution of hb, af, bt, and qz, so that samples with the highest melt fractions have residual pl + qz and new or re-equilibrated af + hyp + aug + mt + il in high-silica rhyolitic glass (75-77% SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>). Mineral compositions vary systematically with increasing temperature. Hornblende is absent in rocks with Fe-Ti oxide temperatures >870°C, and bt above 970°C. Oxygen isotope fractionation between qz, pl, and glass in partially fused granodiorite also is consistent with equilibration at T≥900°C (Δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O\u003Cjats:sub>qz.pl\u003C\u002Fjats:sub> = +0·7 ± 0·5‰). Element partitioning between glass and crystals reflects the large fraction of refractory pl, re-equilibration of af and isolation or incomplete dissolution of accessory phases. Ba and REE contents of analysed glass separates can be successfully modelled by observed degrees of partial melting of granodiorite, but Rb, Sr and Sc concentrations cannot. Several samples have veins of microlite-free glass 1–5 mm thick that are compositionally and physically continuous with intergranular melt and which apparently formed after the climactic eruption began. Whole-rock H\u003Cjats:sub>2\u003C\u002Fjats:sub>O content, microprobe glass analysis sums near 100% and evidence for high temperature suggest liquids in the hotter samples were nearly anhydrous. The occurrence of similar granodiorite blocks at all azimuths around the 8 × 10 km caldera implies derivation from one pluton. Compositional similarity between granodiorite and pre-Mazama rhyodacites suggests that the pluton may have crystallised as recently as 0·4 Ma; compositional data preclude crystallisation from the Holocene chamber. The history of crystallisation, hydrothermal alteration, and remelting of the granitic rocks may be characteristic of shallow igneous systems in which the balance between hydrothermal cooling and magmatic input changes repeatedly over intervals of 10\u003Cjats:sup>4\u003C\u002Fjats:sup>-10\u003Cjats:sup>6\u003C\u002Fjats:sup> years.\u003C\u002Fjats:p>",{"EN":124},"Partially melted granodiorite and related rocks ejected from Crater Lake caldera, Oregon",{"VOID":126},"10.1017\u002Fs0263593300007732","PUBLICATION","VERIFIED","2024-09-21T21:24:58.928+00:00","Auto Verify",[132],"EN","https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0263593300007732\u002Ftype\u002Fjournal_article",[135],{"id":136,"sortIndex":25,"researcher":24,"roles":137,"affiliations":138,"properties":149},"2acfb21b-0839-45f7-96a6-fda3e5231d77",[],[139],{"id":140,"sortIndex":25,"affiliation":141,"properties":24},"ded67ff3-3c04-4f4c-b461-0b0e4de1cbc5",{"id":142,"createTime":143,"updateTime":143,"relativeEntities":144,"slug":145,"properties":146,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"ce198e2c-aeef-4064-bdd0-d1d22b561f7a","2024-09-21T21:24:58.946+00:00",[],"Charles-R-Bacon-U-S-Geological-Survey-MS-910-345-Middlefield-Road-Menlo-Park-California-94025-3591-U-S-A-",{"title":147},{"EN":148},"Charles R. Bacon, U.S. Geological Survey MS 910,345 Middlefield Road, Menlo Park, California 94025-3591, U.S.A.",{"openalex":150,"orcid":152,"title":154},{"VOID":151},"A5019637055",{"VOID":153},"https:\u002F\u002Forcid.org\u002F0000-0002-2165-5618",{"EN":155},"Charles R. Bacon","ARTICLE",{"url":24,"publisher":158,"properties":183},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":159,"slug":10,"properties":160,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":166,"manageAffiliations":167,"indexDatabases":168,"url":107,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":161,"issn":162,"introduce":163,"eissn":164,"title":165},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[169,176],{"id":68,"indexDatabase":170,"url":83,"indexYears":24,"academicFieldIds":175,"indexDatabaseRanking":24},{"id":70,"createTime":71,"updateTime":72,"relativeEntities":171,"label":172,"description":173,"key":79,"publicationTags":174,"standard":24},[],{"EN":75,"VI":75},{"VI":77,"EN":78},[81,82],[85,86],{"id":88,"indexDatabase":177,"url":101,"indexYears":102,"academicFieldIds":182,"indexDatabaseRanking":106},{"id":90,"createTime":91,"updateTime":92,"relativeEntities":178,"label":179,"description":180,"key":98,"publicationTags":181,"standard":24},[],{"EN":95,"VI":95},{"EN":95,"VI":97},[100],[104,105],{"volume":184,"pages":186,"issue":188},{"VOID":185},"83",{"VOID":187},"27-47",{"VOID":189},"1-2",27,{"total":190,"publishYear":24,"statisticByYear":192},{"2012":53,"2015":193,"2017":64},1,"1992-01-01",1992,[197,200,203,206,209,212,215,218,221,224,227,230,233,236,239,242,245,248,251,254,257,260,263,266,269,272,275,278,281,284,287,290,293,296,299,302,305,308,311,314,317,320,323,326,329,332,335,338,341,344,347,350,353,356,359,362,365,368,371,374,377,380,383,386,389,392,395,398],{"id":24,"text":198,"url":24,"identifiers":199},"Andersen, 1988, Internally consistent solution models for Fe–Mg–Mn–Ti oxides: Fe-Ti oxides, AM MINERAL, 73, 714",{},{"id":24,"text":201,"url":24,"identifiers":202},"Lidstrom J. W. Jr 1971. A new model for the formation of Crater Lake caldera, Oregon. Ph.D. Dissertation, Oregon State University.",{},{"id":24,"text":204,"url":24,"identifiers":205},"10.1144\u002Fgsjgs.144.2.0281",{"doi":204},{"id":24,"text":207,"url":24,"identifiers":208},"10.1093\u002Fpetrology\u002F15.2.403",{"doi":207},{"id":24,"text":210,"url":24,"identifiers":211},"10.1016\u002F0016-7037(91)90029-5",{"doi":210},{"id":24,"text":213,"url":24,"identifiers":214},"10.1016\u002F0012-821X(89)90132-5",{"doi":213},{"id":24,"text":216,"url":24,"identifiers":217},"Nekvasil, 1988, Calculated effect of anorthite component on the crystallization paths of H2O-undersaturated haplogranitic melts, AM MINERAL, 73, 966",{},{"id":24,"text":219,"url":24,"identifiers":220},"10.1016\u002F0040-1951(77)90005-1",{"doi":219},{"id":24,"text":222,"url":24,"identifiers":223},"Fiske, 1963, The geology of Mount Rainier National Park, Washington, US GEOL SURV PROF PAP, 444",{},{"id":24,"text":225,"url":24,"identifiers":226},"10.1016\u002F0012-821X(81)90144-8",{"doi":225},{"id":24,"text":228,"url":24,"identifiers":229},"Taylor, 1968, Accidental plutonic ejecta at Crater Lake, Oregon, GEOL SOC AM SPEC PAP, 115, 221",{},{"id":24,"text":231,"url":24,"identifiers":232},"10.1016\u002F0016-7037(85)90231-5",{"doi":231},{"id":24,"text":234,"url":24,"identifiers":235},"10.1007\u002FBF00370985",{"doi":234},{"id":24,"text":237,"url":24,"identifiers":238},"Ritchey J. L. 1979. Origin of divergent magmas at Crater Lake, Oregon. Ph.D. Dissertation, University of Oregon.",{},{"id":24,"text":240,"url":24,"identifiers":241},"10.2475\u002Fajs.283.10.993",{"doi":240},{"id":24,"text":243,"url":24,"identifiers":244},"10.1093\u002Fpetrology\u002F25.3.713",{"doi":243},{"id":24,"text":246,"url":24,"identifiers":247},"10.1029\u002FJB086iB11p10193",{"doi":246},{"id":24,"text":249,"url":24,"identifiers":250},"10.1016\u002F0016-7037(91)90004-O",{"doi":249},{"id":24,"text":252,"url":24,"identifiers":253},"10.1093\u002Fpetrology\u002F30.3.711",{"doi":252},{"id":24,"text":255,"url":24,"identifiers":256},"10.1017\u002FS0263593300014243",{"doi":255},{"id":24,"text":258,"url":24,"identifiers":259},"Halliday, Modelling the petrogenesis of high Rb\u002FSr silicic magmas, CHEM GEOL, 92, 1991",{},{"id":24,"text":261,"url":24,"identifiers":262},"10.1007\u002FBF00375365",{"doi":261},{"id":24,"text":264,"url":24,"identifiers":265},"Elkins, 1990, Ternary feldspar experiments and thermodynamic models, AM MINERAL, 75, 544",{},{"id":24,"text":267,"url":24,"identifiers":268},"10.1016\u002F0377-0273(86)90038-7",{"doi":267},{"id":24,"text":270,"url":24,"identifiers":271},"Dodge, 1978, Fusion of granodiorite by basalt, central Sierra Nevada, J RES US GEOL SURV, 6, 459",{},{"id":24,"text":273,"url":24,"identifiers":274},"10.1016\u002F0016-7037(91)90411-W",{"doi":273},{"id":24,"text":276,"url":24,"identifiers":277},"Bacon, 1992, AM MINERAL",{},{"id":24,"text":279,"url":24,"identifiers":280},"10.1016\u002F0377-0273(83)90004-5",{"doi":279},{"id":24,"text":282,"url":24,"identifiers":283},"Bacon, 1988, Mg\u002FMn partitioning as a test for equilibrium between coexisting Fe–Ti oxides, AM MINERAL, 73, 57",{},{"id":24,"text":285,"url":24,"identifiers":286},"10.1007\u002FBF00371707",{"doi":285},{"id":24,"text":288,"url":24,"identifiers":289},"10.1016\u002F0012-821X(78)90123-1",{"doi":288},{"id":24,"text":291,"url":24,"identifiers":292},"Huebner, 1970, The oxygen fugacity-temperature relationships of manganese oxide and nickel oxide buffers, AM MINERAL, 55, 934",{},{"id":24,"text":294,"url":24,"identifiers":295},"10.1007\u002FBF01132331",{"doi":294},{"id":24,"text":297,"url":24,"identifiers":298},"10.1017\u002FS0263593300014280",{"doi":297},{"id":24,"text":300,"url":24,"identifiers":301},"10.1007\u002FBF00402914",{"doi":300},{"id":24,"text":303,"url":24,"identifiers":304},"10.1007\u002FBF00375310",{"doi":303},{"id":24,"text":306,"url":24,"identifiers":307},"10.1007\u002FBF00375359",{"doi":306},{"id":24,"text":309,"url":24,"identifiers":310},"10.1016\u002F0012-821X(83)90211-X",{"doi":309},{"id":24,"text":312,"url":24,"identifiers":313},"10.1017\u002FS0263593300014176",{"doi":312},{"id":24,"text":315,"url":24,"identifiers":316},"10.1007\u002FBF00457293",{"doi":315},{"id":24,"text":318,"url":24,"identifiers":319},"Bacon, 1990, PAC DIV AM ASSOC ADV SCI, 19",{},{"id":24,"text":321,"url":24,"identifiers":322},"10.1016\u002F0040-1951(78)90069-0",{"doi":321},{"id":24,"text":324,"url":24,"identifiers":325},"10.1007\u002FBF00402114",{"doi":324},{"id":24,"text":327,"url":24,"identifiers":328},"Diller, 1902, The geology and petrography of Crater Lake National Park, US GEOL SURV PROF PAP, 3",{},{"id":24,"text":330,"url":24,"identifiers":331},"Crank, 1975, The Mathematics of Diffusion",{},{"id":24,"text":333,"url":24,"identifiers":334},"10.1007\u002FBF00951335",{"doi":333},{"id":24,"text":336,"url":24,"identifiers":337},"10.1130\u002F0091-7613(1989)017\u003C0837:ECOTAI>2.3.CO;2",{"doi":336},{"id":24,"text":339,"url":24,"identifiers":340},"Liu M. & Yund R. A. 1992. NaSi-CaAl interdiffusion in plagioclase. AM MINERAL (in press).",{},{"id":24,"text":342,"url":24,"identifiers":343},"10.1016\u002F0016-7037(84)90403-4",{"doi":342},{"id":24,"text":345,"url":24,"identifiers":346},"Hollister, 1987, Confirmation of the empirical correlation of Al in hornblende with pressure of solidification of calc-alkaline plutons, AM MINERAL, 72, 231",{},{"id":24,"text":348,"url":24,"identifiers":349},"Chou, 1978, Calibration of oxygen buffers at elevated pressure and temperature using the hydrogen fugacity sensor, AM MINERAL, 63, 650",{},{"id":24,"text":351,"url":24,"identifiers":352},"10.1029\u002FJB089iB10p08339",{"doi":351},{"id":24,"text":354,"url":24,"identifiers":355},"Tuttle, 1958, Origin of granite in the light of experimental studies in the system NaAlSi3O8—KAlSi3O8—SiO2—H2O, GEOL SOC AM MEM, 74",{},{"id":24,"text":357,"url":24,"identifiers":358},"10.1086\u002F629193",{"doi":357},{"id":24,"text":360,"url":24,"identifiers":361},"10.1016\u002F0016-7037(70)90009-8",{"doi":360},{"id":24,"text":363,"url":24,"identifiers":364},"Watson, 1987, Contiguity and the rheology of partially molten granitoids, EOS, 68, 1143",{},{"id":24,"text":366,"url":24,"identifiers":367},"Al-Rawi, 1967, A note on the natural fusion of granite, AM MINERAL, 52, 1086",{},{"id":24,"text":369,"url":24,"identifiers":370},"Stomer, 1983, The effects of recalculation on estimates of temperature and oxygen fugacity from analyses of multicomponent iron-titanium oxides, AM MINERAL, 68, 586",{},{"id":24,"text":372,"url":24,"identifiers":373},"10.1016\u002F0016-7037(84)90391-0",{"doi":372},{"id":24,"text":375,"url":24,"identifiers":376},"10.2475\u002Fajs.272.9.870",{"doi":375},{"id":24,"text":378,"url":24,"identifiers":379},"10.1007\u002F978-1-4613-2347-1_2",{"doi":378},{"id":24,"text":381,"url":24,"identifiers":382},"10.1016\u002F0016-7037(91)90129-S",{"doi":381},{"id":24,"text":384,"url":24,"identifiers":385},"10.1093\u002Fpetrology\u002F31.1.135",{"doi":384},{"id":24,"text":387,"url":24,"identifiers":388},"Lu, 1991, Mixing origins of volatile and thermal gradients in the Bishop magma, EOS, 72, 312",{},{"id":24,"text":390,"url":24,"identifiers":391},"10.1016\u002F0016-7037(85)90002-X",{"doi":390},{"id":24,"text":393,"url":24,"identifiers":394},"10.1007\u002FBF00399362",{"doi":393},{"id":24,"text":396,"url":24,"identifiers":397},"Williams, 1942, The geology of Crater Lake National Park, Oregon, CARNEGIE INST WASHINGTON PUBL, 540",{},{"id":24,"text":399,"url":24,"identifiers":400},"10.1007\u002FBF00373672",{"doi":399},false,{"id":403,"createTime":404,"updateTime":404,"relativeEntities":405,"slug":406,"properties":407,"entityType":127,"verifyStatus":23,"verifyTime":404,"verifyNote":417,"syncStatus":23,"languages":418,"translateLanguages":24,"viewCount":25,"primaryUrl":419,"fullTextUrl":24,"authors":420,"publicationType":156,"publisherRelationship":449,"citationCount":480,"citationInfo":481,"publishDate":194,"publishYear":195,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":495,"isForceReanalyzing":401},"23c571ec-2d19-4032-923e-dd3f86823528","2024-09-29T14:36:52.677+00:00",[],"I-and-S-type-granites-in-the-Lachlan-Fold-Belt",{"keywords":408,"openalex":409,"abstract":411,"title":413,"doi":415},{},{"VOID":410},"W4255137559",{"EN":412},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>Granites and related volcanic rocks of the Lachlan Fold Belt can be grouped into suites using chemical and petrographic data. The distinctive characteristics of suites reflect source-rock features. The first-order subdivision within the suites is between those derived from igneous and from sedimentary source rocks, the I- and S-types. Differences between the two types of source rocks and their derived granites are due to the sedimentary source material having been previously weathered at the Earth's surface. Chemically, the S-type granites are lower in Na, Ca, Sr and Fe\u003Cjats:sup>3+\u003C\u002Fjats:sup>\u002FFe\u003Cjats:sup>2+\u003C\u002Fjats:sup>, and higher in Cr and Ni. As a consequence, the S-types are always peraluminous and contain Al-rich minerals. A little over 50% of the I-type granites are metaluminous and these more mafic rocks contain hornblende. In the absence of associated mafic rocks, the more felsic and slightly peraluminous I-type granites may be difficult to distinguish from felsic S-type granites. This overlap in composition is to be expected and results from the restricted chemical composition of the lowest temperature felsic melts. The compositions of more mafic I- and S-type granites diverge, as a result of the incorporation of more mafic components from the source, either as restite or a component of higher temperature melt. There is no overlap in composition between the most mafic I- and S-type granites, whose compositions are closest to those of their respective source rocks. Likewise, the enclaves present in the more mafic granites have compositions reflecting those of their host rocks, and probably in most cases, the source rocks.\u003C\u002Fjats:p>\u003Cjats:p>S-type granites have higher δ\u003Cjats:sup>18\u003C\u002Fjats:sup>O values and more evolved Sr and Nd isotopic compositions, although the radiogenic isotope compositions overlap with I-types. Although the isotopic compositions lie close to a mixing curve, it is thought that the amount of mixing in the source rocks was restricted, and occurred prior to partial melting. I-type granites are thought to have been derived from deep crust formed by underplating and thus are infracrustal, in contrast to the supracrustal S-type source rocks.\u003C\u002Fjats:p>\u003Cjats:p>Crystallisation of feldspars from felsic granite melts leads to distinctive changes in the trace element compositions of more evolved I- and S-type granites. Most notably, P increases in abundance with fractionation of crystals from the more strongly peraluminous S-type felsic melts, while it decreases in abundance in the analogous, but weakly peraluminous, I-type melts.\u003C\u002Fjats:p>",{"EN":414},"I- and S-type granites in the Lachlan Fold Belt",{"VOID":416},"10.1017\u002Fs0263593300007720","Author affiliation is blank",[132],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0263593300007720\u002Ftype\u002Fjournal_article",[421,430],{"id":422,"sortIndex":193,"researcher":24,"roles":423,"affiliations":424,"properties":425},"37c78133-7aee-450c-9236-4dd753fef8a9",[],[],{"openalex":426,"title":428},{"VOID":427},"A5013397189",{"EN":429},"A. J. R. White",{"id":431,"sortIndex":25,"researcher":24,"roles":432,"affiliations":433,"properties":444},"d9d609c5-aa61-47bb-8488-44395896f548",[],[434],{"id":435,"sortIndex":25,"affiliation":436,"properties":24},"05a5e4f0-7288-4568-82d8-bf6421e280d8",{"id":437,"createTime":438,"updateTime":438,"relativeEntities":439,"slug":440,"properties":441,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"dae5956f-a564-457c-b996-baad3e4865eb","2024-09-29T14:36:52.691+00:00",[],"B-W-Chappell-and-A-J-R-White-Department-of-Geology-The-Australian-National-University-Canberra-ACT-2601-Australia",{"title":442},{"EN":443},"B. W. Chappell and A. J. R. White, Department of Geology, The Australian National University, Canberra ACT 2601, Australia",{"openalex":445,"title":447},{"VOID":446},"A5062931133",{"EN":448},"B. W. Chappell",{"url":24,"publisher":450,"properties":475},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":451,"slug":10,"properties":452,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":458,"manageAffiliations":459,"indexDatabases":460,"url":107,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":453,"issn":454,"introduce":455,"eissn":456,"title":457},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[461,468],{"id":68,"indexDatabase":462,"url":83,"indexYears":24,"academicFieldIds":467,"indexDatabaseRanking":24},{"id":70,"createTime":71,"updateTime":72,"relativeEntities":463,"label":464,"description":465,"key":79,"publicationTags":466,"standard":24},[],{"EN":75,"VI":75},{"VI":77,"EN":78},[81,82],[85,86],{"id":88,"indexDatabase":469,"url":101,"indexYears":102,"academicFieldIds":474,"indexDatabaseRanking":106},{"id":90,"createTime":91,"updateTime":92,"relativeEntities":470,"label":471,"description":472,"key":98,"publicationTags":473,"standard":24},[],{"EN":95,"VI":95},{"EN":95,"VI":97},[100],[104,105],{"volume":476,"pages":477,"issue":479},{"VOID":185},{"VOID":478},"1-26",{"VOID":189},1423,{"total":480,"publishYear":24,"statisticByYear":482},{"2012":483,"2013":484,"2014":485,"2015":486,"2016":487,"2017":488,"2018":489,"2019":490,"2020":491,"2021":492,"2022":493,"2023":488,"2024":494},26,42,53,50,75,91,110,123,139,143,120,70,[496,499,502,505,508,511,514,517,520,523,526,529,532,535,538,541,544,547,550,553,556,559,562,565,568,571,574,577,580,583,586,589,592,595,598,601,604,607,611,614,617,620,623,626,629,632,635,638,641,644,647,650,653,656,659,662,665,668,671,674,677,680,683,686,689,692,695,698,701,704,707,710,713,715,718,721,724,727,730,733,736,739,742,745,749,752,755,758,761,764,767,770,773,776,779,782],{"id":24,"text":497,"url":24,"identifiers":498},"10.1017\u002FS0263593300008051",{"doi":497},{"id":24,"text":500,"url":24,"identifiers":501},"10.1017\u002FS026359330001419X",{"doi":500},{"id":24,"text":503,"url":24,"identifiers":504},"10.1080\u002F14400957308527908",{"doi":503},{"id":24,"text":506,"url":24,"identifiers":507},"Williams I. S. 1973. Granites north of Jindabyne, New South Wales. Unpublished BSc thesis, The Australian National University.",{},{"id":24,"text":509,"url":24,"identifiers":510},"Baker, 1940, Cordierite granite from Terip Terip, Victoria, AM MINERAL, 25, 543",{},{"id":24,"text":512,"url":24,"identifiers":513},"10.1017\u002FS026359330000780X",{"doi":512},{"id":24,"text":515,"url":24,"identifiers":516},"Chappell B. W. , Williams I. S. , White A. J. R. & McCulloch M. T. , 1990. Granites of the Lachlan Fold Belt. ICOG 7 Field Guide Excursion A-2. REC BMR GEOL GEOPHYS 1990\u002F48.",{},{"id":24,"text":518,"url":24,"identifiers":519},"10.1007\u002FBF00457291",{"doi":518},{"id":24,"text":521,"url":24,"identifiers":522},"Chappell, 1974, Two contrasting granite types, PACIFIC GEOL, 8, 173",{},{"id":24,"text":524,"url":24,"identifiers":525},"10.1080\u002F00167617608728936",{"doi":524},{"id":24,"text":527,"url":24,"identifiers":528},"White, 1983, circum-Pacific Plutonic Terranes, GEOL SOC AM MEM, 159, 21",{},{"id":24,"text":530,"url":24,"identifiers":531},"Takahashi, 1980, Magnetite-series\u002FIlmenite-series vs I-type\u002FS-type granitoids, MINING GEOL SPEC ISSUE, 8, 13",{},{"id":24,"text":533,"url":24,"identifiers":534},"Chappell, 1991, Granites and related rocks of the Lachlan Fold Belt (1:1 250 000 scale map)",{},{"id":24,"text":536,"url":24,"identifiers":537},"10.1080\u002F08120098808729454",{"doi":536},{"id":24,"text":539,"url":24,"identifiers":540},"10.1144\u002Fgsjgs.133.6.0559",{"doi":539},{"id":24,"text":542,"url":24,"identifiers":543},"Shand, 1927, Eruptive rocks",{},{"id":24,"text":545,"url":24,"identifiers":546},"10.1080\u002F00167617808729030",{"doi":545},{"id":24,"text":548,"url":24,"identifiers":549},"10.1080\u002F00167616208728514",{"doi":548},{"id":24,"text":551,"url":24,"identifiers":552},"10.1002\u002Fgj.3350250306",{"doi":551},{"id":24,"text":554,"url":24,"identifiers":555},"King P. L. , White A. J. R. & Chappell B. W. (in prep.) Characterization and origin of the A-type granites of the Lachlan Fold Belt.",{},{"id":24,"text":557,"url":24,"identifiers":558},"10.1080\u002F00167616508728583",{"doi":557},{"id":24,"text":560,"url":24,"identifiers":561},"Browne, 1929, An outline of the history of igneous activity in New South Wales till the close of the Palaeozoic Era, PROC LINN SOC NSW, 54, 9",{},{"id":24,"text":563,"url":24,"identifiers":564},"McCulloch, 1982, ABST ICOG, 5, 246",{},{"id":24,"text":566,"url":24,"identifiers":567},"10.1007\u002FBF00379742",{"doi":566},{"id":24,"text":569,"url":24,"identifiers":570},"10.1016\u002F0009-2541(83)90073-6",{"doi":569},{"id":24,"text":572,"url":24,"identifiers":573},"10.1093\u002Fpetrology\u002F26.3.603",{"doi":572},{"id":24,"text":575,"url":24,"identifiers":576},"10.1016\u002F0012-821X(82)90102-9",{"doi":575},{"id":24,"text":578,"url":24,"identifiers":579},"Chappell, 1991, Enclaves and Granite Petrology, 375",{},{"id":24,"text":581,"url":24,"identifiers":582},"Joplin, 1942, Petrological studies in the Ordovician of N.S.W. I. The Cooma Complex, PROC LINN SOC NSW, 67, 156",{},{"id":24,"text":584,"url":24,"identifiers":585},"Mysen, 1989, Redox equilibria, structure, and properties of Fe-bearing aluminosilicate melts: relationships among temperature, composition, and oxygen fugacity in the system Na2O–Al2O3,–SiO2–Fe–O, AM MINER, 74, 58",{},{"id":24,"text":587,"url":24,"identifiers":588},"Chappell B. W. & Hine R. (in prep.) Geochemistry and petrogenesis of the Cornubian Batholith.",{},{"id":24,"text":590,"url":24,"identifiers":591},"10.1130\u002FSPE241-p145",{"doi":590},{"id":24,"text":593,"url":24,"identifiers":594},"10.1016\u002F0016-7037(90)90056-Q",{"doi":593},{"id":24,"text":596,"url":24,"identifiers":597},"10.1080\u002F08120098808729466",{"doi":596},{"id":24,"text":599,"url":24,"identifiers":600},"Compston, 1979, The Earth: its origin, structure and evolution, 377",{},{"id":24,"text":602,"url":24,"identifiers":603},"Clemens, 1981, Crystallization and origin of some peraluminous (S-type) granite magmas, CAN MINERAL, 19, 111",{},{"id":24,"text":605,"url":24,"identifiers":606},"Chappell B. W. , Wyborn L. A. I. , White A. J. R. , Burnham C. W. & Wyborn D. (in prep.) S-type granites of the Wagga Basement Terrane: an example of compositional variation resulting from sequential restite fractionation, fractional crystallization and hydrothermal alteration.",{},{"id":24,"text":608,"url":24,"identifiers":609},"Bateman P. C. , Clark L. D. , Huber N. K. , Moore J. G. & Rinehart C. D. 1963. The Sierra Nevada Batholith: a synthesis of recent work across the central part. US GEOL SURV PROF PAP 414D.",{"doi":610},"10.3133\u002Fpp414D",{"id":24,"text":612,"url":24,"identifiers":613},"10.1093\u002Fpetrology\u002F6.2.193",{"doi":612},{"id":24,"text":615,"url":24,"identifiers":616},"Chappell, 1990, Possible mixed source rocks in the Bega Batholith: constraints provided by combined chemical and isotopic studies, ICOG-7, ABST GEOL SOC AUST, 27, 17",{},{"id":24,"text":618,"url":24,"identifiers":619},"10.1017\u002FS0263593300014152",{"doi":618},{"id":24,"text":621,"url":24,"identifiers":622},"David, 1950, The Geology of the Commonwealth of Australia",{},{"id":24,"text":624,"url":24,"identifiers":625},"10.1080\u002F00167617808729035",{"doi":624},{"id":24,"text":627,"url":24,"identifiers":628},"Whalen, 1988, Opaque mineralogy and mafic mineral chemistry of I- and S-type granites of the Lachlan Fold Belt, southeast Australia, AM MINERAL, 73, 281",{},{"id":24,"text":630,"url":24,"identifiers":631},"Chappell, 1984, Geology of granites and their metallogenic relations, 87",{},{"id":24,"text":633,"url":24,"identifiers":634},"10.1029\u002FJB095iB11p17757",{"doi":633},{"id":24,"text":636,"url":24,"identifiers":637},"White, 1977, Geology of the Berridale 1:100000 Sheet (8625)",{},{"id":24,"text":639,"url":24,"identifiers":640},"MacKenzie, Origin of alkali-feldspar granites: an example from the Poimena Granite, northweastern Tasmania, Australia”, GEOCHIM COSMOCHIM ACTA, 54, 1990",{},{"id":24,"text":642,"url":24,"identifiers":643},"Wones, 1989, Significance of the assemblage titanite + magnetite + quartz in granitic rocks, AM MINERAL, 74, 744",{},{"id":24,"text":645,"url":24,"identifiers":646},"10.1080\u002F00167617508728914",{"doi":645},{"id":24,"text":648,"url":24,"identifiers":649},"Williams, 1988, Dating the sources of Bega Batholith granites by ion microprobe, ABST GEOL SOC AUST, 21, 424",{},{"id":24,"text":651,"url":24,"identifiers":652},"Chappell B. W. & White A. J. R. 1976. Plutonic rocks of the Lachlan Mobile Zone. International Geological Congress 25, Field Guide Excursion 13C.",{},{"id":24,"text":654,"url":24,"identifiers":655},"10.1080\u002F00167616608728603",{"doi":654},{"id":24,"text":657,"url":24,"identifiers":658},"Wyborn D. 1983. Fractionation processes in the Boggy Plain zoned pluton. Unpublished PhD thesis, The Australian National University.",{},{"id":24,"text":660,"url":24,"identifiers":661},"10.1029\u002FJB086iB11p10335",{"doi":660},{"id":24,"text":663,"url":24,"identifiers":664},"10.1080\u002F08120098708729392",{"doi":663},{"id":24,"text":666,"url":24,"identifiers":667},"10.1017\u002FS0263593300007987",{"doi":666},{"id":24,"text":669,"url":24,"identifiers":670},"Joyce A. S. 1970. Geochemistry of the Murrumbidgee Batholith. Unpublished PhD thesis, The Australian National University.",{},{"id":24,"text":672,"url":24,"identifiers":673},"10.1017\u002FS001675680009155X",{"doi":672},{"id":24,"text":675,"url":24,"identifiers":676},"Montel, 1988, High apatite solubility in peraluminous melts, TERRA COGNITA, 8, 71",{},{"id":24,"text":678,"url":24,"identifiers":679},"10.1130\u002F0016-7606(1973)84\u003C3181:FRITSN>2.0.CO;2",{"doi":678},{"id":24,"text":681,"url":24,"identifiers":682},"Reid, 1983, Petrogenesis of the Murrumbucka Tonalite: a granitoid with both I- and S-type character, ABST GEOL SOC AUST, 9, 179",{},{"id":24,"text":684,"url":24,"identifiers":685},"White, 1974, Geologic setting and emplacement of some Australian Palaeozoic batholiths and implications for intrusive mechanisms, PACIFIC GEOL, 8, 159",{},{"id":24,"text":687,"url":24,"identifiers":688},"Ishihara, 1977, The magnetite-series and ilmenite-series granitic rocks, MINING GEOL, 27, 293",{},{"id":24,"text":690,"url":24,"identifiers":691},"White, Berridale 1:100000 Geological Sheet",{},{"id":24,"text":693,"url":24,"identifiers":694},"10.1093\u002Fpetrology\u002F27.5.1095",{"doi":693},{"id":24,"text":696,"url":24,"identifiers":697},"10.1098\u002Frsta.1984.0015",{"doi":696},{"id":24,"text":699,"url":24,"identifiers":700},"10.1080\u002F08120099008727931",{"doi":699},{"id":24,"text":702,"url":24,"identifiers":703},"10.1093\u002Fpetrology\u002F28.6.1111",{"doi":702},{"id":24,"text":705,"url":24,"identifiers":706},"Tetley N. W. 1978. Geochronology by the 40Ar\u002F39Ar technique using HIFAR reactor. Unpublished PhD thesis, The Australian National University.",{},{"id":24,"text":708,"url":24,"identifiers":709},"10.2475\u002Fajs.245.7.401",{"doi":708},{"id":24,"text":711,"url":24,"identifiers":712},"10.1007\u002FBF00374895",{"doi":711},{"id":24,"text":306,"url":24,"identifiers":714},{"doi":306},{"id":24,"text":716,"url":24,"identifiers":717},"10.1016\u002F0012-821X(77)90008-5",{"doi":716},{"id":24,"text":719,"url":24,"identifiers":720},"Chappell B. W. 1966. Petrogenesis of the granites at Moonbi, New South Wales. Unpublished PhD thesis, The Australian National University.",{},{"id":24,"text":722,"url":24,"identifiers":723},"10.1080\u002F00167616208728515",{"doi":722},{"id":24,"text":725,"url":24,"identifiers":726},"Hine R. 1971. Granite studies of the Kosciusko Batholith. Unpublished BSc thesis, The Australian National University.",{},{"id":24,"text":728,"url":24,"identifiers":729},"10.1016\u002F0012-821X(84)90208-5",{"doi":728},{"id":24,"text":731,"url":24,"identifiers":732},"White, 1989, Geology of the Numbla 1:100 000 Sheet (8624)",{},{"id":24,"text":734,"url":24,"identifiers":735},"10.1093\u002Fpetrology\u002F13.1.1",{"doi":734},{"id":24,"text":737,"url":24,"identifiers":738},"10.1130\u002F0016-7606(1965)76[165:IOISSR]2.0.CO;2",{"doi":737},{"id":24,"text":740,"url":24,"identifiers":741},"Tuttle, 1958, Origin of granite in the light of experimental studies in the system NaAlSi3O8–KAlSi2O8–SiO2–H2O, GEOL SOC AM MEM, 74",{},{"id":24,"text":743,"url":24,"identifiers":744},"MacKenzie, 1988, GEOCHIM COSMOCHIM ACTA, 52, 2507",{},{"id":24,"text":746,"url":24,"identifiers":747},"Read, 1949, A contemplation of time in plutonism, Q J GEOL SOC LONDON, 105, 101, 10.1144\u002FGSL.JGS.1949.105.01-04.06",{"doi":748},"10.1144\u002FGSL.JGS.1949.105.01-04.06",{"id":24,"text":750,"url":24,"identifiers":751},"10.1080\u002F00167617808729029",{"doi":750},{"id":24,"text":753,"url":24,"identifiers":754},"10.1130\u002FMEM28-p1",{"doi":753},{"id":24,"text":756,"url":24,"identifiers":757},"Vallance, 1969, Southern and Central Highlands fold belt: plutonic and metamorphic rocks, J GEOL SOC AUST, 16, 180",{},{"id":24,"text":759,"url":24,"identifiers":760},"Chappell, 1979, Granites as images of their source rocks, GEOL SOC AMERICA PROG ABST, 11, 400",{},{"id":24,"text":762,"url":24,"identifiers":763},"Tattam, 1925, Contact metamorphism in the Bulla area, PROC R SOC VICTORIA, 37, 230",{},{"id":24,"text":765,"url":24,"identifiers":766},"Ball C. W. , Dallwitz W. B. & Noakes L. C. 1948. Geological reconnaissance of the proposed hydro-electric works in Kosciusko area between Waste Point and Khancoban. REC BMR GEOL GEOPHYS 1948\u002F7.",{},{"id":24,"text":768,"url":24,"identifiers":769},"White, 1989, Numbla 1:100 000 Geological Sheet",{},{"id":24,"text":771,"url":24,"identifiers":772},"Reid E. J. 1980. The geology and geochemistry of the Murrumbucka region. Unpublished MSc thesis, The Australian National University.",{},{"id":24,"text":774,"url":24,"identifiers":775},"Chen, 1991, Enclaves and granite petrology, 113",{},{"id":24,"text":777,"url":24,"identifiers":778},"10.1017\u002FS0263593300014139",{"doi":777},{"id":24,"text":780,"url":24,"identifiers":781},"Browne, 1931, Notes on bathyliths and some of their implications, J R SOC NSW, 65, 114",{},{"id":24,"text":783,"url":24,"identifiers":784},"10.1016\u002F0040-1951(77)90003-8",{"doi":783},{"id":786,"createTime":787,"updateTime":787,"relativeEntities":788,"slug":789,"properties":790,"entityType":127,"verifyStatus":128,"verifyTime":787,"verifyNote":130,"syncStatus":23,"languages":800,"translateLanguages":24,"viewCount":25,"primaryUrl":801,"fullTextUrl":24,"authors":802,"publicationType":156,"publisherRelationship":822,"citationCount":853,"citationInfo":854,"publishDate":194,"publishYear":195,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":863,"isForceReanalyzing":401},"c326a6f0-7a36-463e-8ed0-55e2a0c7020e","2024-10-07T10:31:30.569+00:00",[],"Controls-on-ore-metal-ratios-in-granite-related-ore-systems-an-experimental-and-computational-approach",{"keywords":791,"openalex":792,"abstract":794,"title":796,"doi":798},{},{"VOID":793},"W4240887009",{"EN":795},"\u003Cjats:title>ABSTRACT\u003C\u002Fjats:title>\u003Cjats:p>Size and composition (bulk metal ratios) of magmatic hydrothermal mineral deposits are affected by a number of chemical and physical processes including the nature of the source region and mode of emplacement. At shallow levels, rising plumes of vapour bubbles + melt, and the advection of water through interconnected vapour bubbles, allows access of the magmatic aqueous phase to the upper reaches of a magma chamber. These processes are operative at shallow levels where low water solubility and high molar volume for water make these processes more efficient.\u003C\u002Fjats:p>\u003Cjats:p>Partitioning experiments suggest that oxygen fugacity-dependent crystal\u002Fmelt partitioning of ore metals leads to different efficiencies of removal of Cu, W, and Mo from silicate melts into ore-forming aqueous fluids. For example, the Mo\u002FW ratio in magmatic hydrothermal deposits should increase as the oxygen fugacity of the magma increases. Further, Cu should behave as a crystal-compatible element in H\u003Cjats:sub>2\u003C\u002Fjats:sub>O-undersaturated, sulfide-saturated felsic magmas with \u003Cjats:italic>f\u003Cjats:sub>O\u003C\u002Fjats:sub>\u003Cjats:sub>2\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> NNO + 1 due to the strong partitioning of Cu from the melt into pyrrhotite.\u003C\u002Fjats:p>\u003Cjats:p>Cycling of oxidised, hydrated, sulfidised and Cl-enriched oceanic crust into mantle can give rise to magmas that contain S but are oxidised (≥NNO). The combination of high oxidation state, relatively hydrous \u003Cjats:italic>but\u003C\u002Fjats:italic> shallow conditions and a high Cl\u002FH\u003Cjats:sub>2\u003C\u002Fjats:sub>O ratio leads to saturation with respect to H\u003Cjats:sub>2\u003C\u002Fjats:sub>O early during crystallisation, and loss of a large proportion of magmatic Cu to the aqueous phase. Ores formed from these oxidised magmas also possess high Mo\u002FW ratios due to the effect of oxygen fugacity on the sequestering of Mo vs W.\u003C\u002Fjats:p>\u003Cjats:p>In less oxidised magmas, Cu and Mo are partitioned into sulfides and Ti-bearing phases, respectively, resulting in lower efficiencies of removal of Cu and Mo from melts into aqueous fluids. Further, the partitioning of W into crystallising phases is \u003Cjats:italic>reduced\u003C\u002Fjats:italic>, producing a more efficient removal of W into ore-forming fluids. This ultimately leads to mineral deposits with higher W\u002F(Mo + Cu) ratios relative to deposits associated with more oxidised systems. Silicic, high-F magmas with \u003Cjats:italic>f\u003C\u002Fjats:italic>\u003Cjats:sub>O\u003C\u002Fjats:sub>\u003Cjats:sub>2\u003C\u002Fjats:sub> = NNO can be found in tensional environments (e.g. rocks associated with the Climax-type deposits of the Colorado Mineral Belt). High HF\u002FH\u003Cjats:sub>2\u003C\u002Fjats:sub>O activity ratios in the source regions yield melts that evolve an aqueous phase late during crystallisation, leading to relatively low ratios of compatible\u002Fincompatible elements in the melt at H\u003Cjats:sub>2\u003C\u002Fjats:sub>O saturation.\u003C\u002Fjats:p>",{"EN":797},"Controls on ore metal ratios in granite-related ore systems: an experimental and computational approach",{"VOID":799},"10.1017\u002Fs0263593300007999",[132],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0263593300007999\u002Ftype\u002Fjournal_article",[803],{"id":804,"sortIndex":25,"researcher":24,"roles":805,"affiliations":806,"properties":817},"19ce3d7a-1379-4cd1-9c08-bb790518e371",[],[807],{"id":808,"sortIndex":25,"affiliation":809,"properties":24},"990a330a-7965-44b4-8b6a-f2b8d0e455c5",{"id":810,"createTime":811,"updateTime":811,"relativeEntities":812,"slug":813,"properties":814,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"77fca2fe-bdec-47ee-9e7d-9f838a387ef9","2024-10-07T10:31:30.596+00:00",[],"Philip-A-Candela-Laboratory-for-Mineral-Deposit-Research-Department-of-Geology-University-of-Maryland-College-Park-Maryland-20742-4211-U-S-A",{"title":815},{"EN":816},"Philip A. Candela, Laboratory for Mineral Deposit Research, Department of Geology,University of Maryland, College Park, Maryland, 20742-4211, U.S.A",{"openalex":818,"title":820},{"VOID":819},"A5067810594",{"EN":821},"Philip A. Candela",{"url":24,"publisher":823,"properties":848},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":824,"slug":10,"properties":825,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":831,"manageAffiliations":832,"indexDatabases":833,"url":107,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":826,"issn":827,"introduce":828,"eissn":829,"title":830},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[834,841],{"id":68,"indexDatabase":835,"url":83,"indexYears":24,"academicFieldIds":840,"indexDatabaseRanking":24},{"id":70,"createTime":71,"updateTime":72,"relativeEntities":836,"label":837,"description":838,"key":79,"publicationTags":839,"standard":24},[],{"EN":75,"VI":75},{"VI":77,"EN":78},[81,82],[85,86],{"id":88,"indexDatabase":842,"url":101,"indexYears":102,"academicFieldIds":847,"indexDatabaseRanking":106},{"id":90,"createTime":91,"updateTime":92,"relativeEntities":843,"label":844,"description":845,"key":98,"publicationTags":846,"standard":24},[],{"EN":95,"VI":95},{"EN":95,"VI":97},[100],[104,105],{"volume":849,"pages":850,"issue":852},{"VOID":185},{"VOID":851},"317-326",{"VOID":189},121,{"total":853,"publishYear":24,"statisticByYear":855},{"2012":856,"2013":857,"2014":858,"2015":857,"2016":858,"2017":859,"2018":859,"2019":860,"2020":861,"2021":862,"2022":857,"2023":193,"2024":53},4,8,6,9,12,10,14,[864,867,870,873,876,879,882,885,888,891,894,897,900,903,906,909,912,915,918,921,924,927,930,933,936,939,942,945,948,951,954,957,960,963,966,969,972,975,978,981,984,987,990,993,996,999,1002,1005,1008,1011],{"id":24,"text":865,"url":24,"identifiers":866},"10.1029\u002FJB093iB06p06503",{"doi":865},{"id":24,"text":868,"url":24,"identifiers":869},"van Middelaar, 1990, Ore-bearing granitic systems; Petrogenesis and mineralizing processes, GEOL SOC AM SPEC PAPER, 246, 21",{},{"id":24,"text":871,"url":24,"identifiers":872},"10.2113\u002Fgsecongeo.81.1.1",{"doi":871},{"id":24,"text":874,"url":24,"identifiers":875},"10.2113\u002Fgsecongeo.83.2.266",{"doi":874},{"id":24,"text":877,"url":24,"identifiers":878},"Dingwell, 1988, The structures and properties of fluorine-rich magmas: a review of experimental studies, Recent advances in the geology of granite-related mineral deposits, 39, 1",{},{"id":24,"text":880,"url":24,"identifiers":881},"Barton, 1988, Metamorphism and crustal evolution, western conterminous United States, 7, 110",{},{"id":24,"text":883,"url":24,"identifiers":884},"Andiambololona, 1978, Répartition et comportment des éléments de transition dans les roches volcaniques. I. cuivre et zinc, BULL B.R.G.M, 2, 121",{},{"id":24,"text":886,"url":24,"identifiers":887},"10.2113\u002Fgsecongeo.85.3.633",{"doi":886},{"id":24,"text":889,"url":24,"identifiers":890},"10.1139\u002Fe70-098",{"doi":889},{"id":24,"text":892,"url":24,"identifiers":893},"10.1038\u002F340199a0",{"doi":892},{"id":24,"text":895,"url":24,"identifiers":896},"10.1016\u002F0377-0273(84)90057-X",{"doi":895},{"id":24,"text":898,"url":24,"identifiers":899},"10.1007\u002FBF00372365",{"doi":898},{"id":24,"text":901,"url":24,"identifiers":902},"10.1016\u002F0016-7037(84)90257-6",{"doi":901},{"id":24,"text":904,"url":24,"identifiers":905},"Carten, 1988, Comparison of field-based studies of the Henderson porphyry molybdenum deposit, Colorado, with experimental and theoretical models of porphyry systems, Recent advances in the geology of granite-related mineral deposits, 39, 351",{},{"id":24,"text":907,"url":24,"identifiers":908},"10.1130\u002F0016-7606(1988)100\u003C0912:MAAADO>2.3.CO;2",{"doi":907},{"id":24,"text":910,"url":24,"identifiers":911},"10.2113\u002Fgsecongeo.80.1.148",{"doi":910},{"id":24,"text":913,"url":24,"identifiers":914},"10.1038\u002F323598a0",{"doi":913},{"id":24,"text":916,"url":24,"identifiers":917},"Piccoli, 1991, Spatial variations in model halogen concentrations in magmas based on apatite chemistry: examples from natural systems, GEOL SOC AM ABSTR PROG, 23, 5",{},{"id":24,"text":919,"url":24,"identifiers":920},"10.1130\u002F0091-7613(1983)11\u003C99:ISITFC>2.0.CO;2",{"doi":919},{"id":24,"text":922,"url":24,"identifiers":923},"Candela, 1989, Magmatic ore-forming fluids: thermodynamic and mass transfer calculations of metal concentrations, Ore Deposits Associated with Magmas, Reviews in Economic Geology, 4, 203",{},{"id":24,"text":925,"url":24,"identifiers":926},"Barton, 1990, The nature and origin of Cordilleran magmatism: Boulder Colorado, GEOL SOC AM MEM, 174, 283",{},{"id":24,"text":928,"url":24,"identifiers":929},"10.1038\u002F339613a0",{"doi":928},{"id":24,"text":931,"url":24,"identifiers":932},"10.1016\u002F0016-7037(87)90057-3",{"doi":931},{"id":24,"text":934,"url":24,"identifiers":935},"10.2113\u002Fgsecongeo.82.7.1827",{"doi":934},{"id":24,"text":937,"url":24,"identifiers":938},"Webster, 1990, Ore-bearing granitic systems; Petrogenesis and mineralizing processes, GEOL SOC AM SPEC PAP, 246, 21",{},{"id":24,"text":940,"url":24,"identifiers":941},"10.2113\u002Fgsecongeo.85.1.99",{"doi":940},{"id":24,"text":943,"url":24,"identifiers":944},"10.1093\u002Fpetrology\u002F31.5.1071",{"doi":943},{"id":24,"text":946,"url":24,"identifiers":947},"10.1093\u002Fpetrology\u002F28.5.781",{"doi":946},{"id":24,"text":949,"url":24,"identifiers":950},"10.1007\u002FBF01160186",{"doi":949},{"id":24,"text":952,"url":24,"identifiers":953},"10.1029\u002FJB089iB12p10161",{"doi":952},{"id":24,"text":955,"url":24,"identifiers":956},"Brandeis, 1987, Magmatic processes: physiochemical principles, 307",{},{"id":24,"text":958,"url":24,"identifiers":959},"10.1007\u002F978-1-4612-4928-3_10",{"doi":958},{"id":24,"text":961,"url":24,"identifiers":962},"Candela, 1989, Felsic magmas, volatiles, and metallogenesis, Ore Deposits Associated with Magmas, Reviews in Economic Geology, 4, 223",{},{"id":24,"text":964,"url":24,"identifiers":965},"Candela, 1991, Physics of Aqueous Phase evolution in Plutonic environments, AM MINERAL, 76, 1081",{},{"id":24,"text":967,"url":24,"identifiers":968},"10.1016\u002F0012-821X(81)90220-X",{"doi":967},{"id":24,"text":970,"url":24,"identifiers":971},"Haffty, 1972, Release and migration of molybdenum during the primary crystallization of peralkaline silicic volcanic rocks, ECON GEOL, 70, 857",{},{"id":24,"text":973,"url":24,"identifiers":974},"Jaeger, 1968, Basalts, 503",{},{"id":24,"text":976,"url":24,"identifiers":977},"Lehmann, 1990, Metallogeny of Tin",{},{"id":24,"text":979,"url":24,"identifiers":980},"Lynton, 1990, Experimental determination of copper partitioning between pyrrhotite and high silica rhyolite, GEOL SOC AM ABST PROG, 22, 181",{},{"id":24,"text":982,"url":24,"identifiers":983},"10.1007\u002FBF00373674",{"doi":982},{"id":24,"text":985,"url":24,"identifiers":986},"10.2475\u002Fajs.282.6.808",{"doi":985},{"id":24,"text":988,"url":24,"identifiers":989},"10.1038\u002F333397a0",{"doi":988},{"id":24,"text":991,"url":24,"identifiers":992},"10.1130\u002F0016-7606(1988)100\u003C1720:CCSARI>2.3.CO;2",{"doi":991},{"id":24,"text":994,"url":24,"identifiers":995},"10.2475\u002Fajs.277.8.937",{"doi":994},{"id":24,"text":997,"url":24,"identifiers":998},"10.1093\u002Fpetrology\u002F20.3.421",{"doi":997},{"id":24,"text":1000,"url":24,"identifiers":1001},"Peck, 1977, AM J SCI, 277, 415",{},{"id":24,"text":1003,"url":24,"identifiers":1004},"Sato, 1982, Chaacteristics of tungsten skarns in Japan, two constrasting types, Proc. Symp. W Geol. Jiangxi, China, 1981, 203",{},{"id":24,"text":1006,"url":24,"identifiers":1007},"Taylor, 1988, Degassing of rhyolitic magmas: Hydrogen isotope evidence and implications for magmatic-hydrothermal ore deposits, Recent Advances in the Geology of Granite-Related Mineral Deposits, 39, 33",{},{"id":24,"text":1009,"url":24,"identifiers":1010},"Titley, 1981, Economic Geology 75th Anniversary Volume",{},{"id":24,"text":1012,"url":24,"identifiers":1013},"10.1016\u002F0016-7037(89)90382-7",{"doi":1012},{"id":1015,"createTime":1016,"updateTime":1016,"relativeEntities":1017,"slug":1018,"properties":1019,"entityType":127,"verifyStatus":128,"verifyTime":1016,"verifyNote":130,"syncStatus":23,"languages":1031,"translateLanguages":24,"viewCount":25,"primaryUrl":1032,"fullTextUrl":24,"authors":1033,"publicationType":156,"publisherRelationship":1093,"citationCount":1125,"citationInfo":1126,"publishDate":1138,"publishYear":1139,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1140,"isForceReanalyzing":401},"d5f52004-0a51-4a83-be9d-e37118069bee","2024-09-29T05:19:37.229+00:00",[],"Petrogenesis-of-slab-derived-trondhjemite-tonalite-dacite-adakite-magmas",{"mag":1020,"keywords":1022,"openalex":1023,"abstract":1025,"title":1027,"doi":1029},{"VOID":1021},"2148388790",{},{"VOID":1024},"W2148388790",{"EN":1026},"\u003Cjats:title>ABSTRACT:\u003C\u002Fjats:title>\u003Cjats:p>The prospect of partial melting of the subducted oceanic crust to produce arc magmatism has been debated for over 30 years. Debate has centred on the physical conditions of slab melting and the lack of a definitive, unambiguous geochemical signature and petrogenetic process. Experimental partial melting data for basalt over a wide range of pressures (1–32 kbar) and temperatures (700–1150°C) have shown that melt compositions are primarily trondhjemite–tonalite–dacite (TTD). High-Al (> 15% Al\u003Cjats:sub>2\u003C\u002Fjats:sub>O\u003Cjats:sub>3\u003C\u002Fjats:sub>at the 70% SiO\u003Cjats:sub>2\u003C\u002Fjats:sub>level) TTD melts are produced by high-pressure (≥ 5 kbar) partial melting of basalt, leaving a restite assemblage of garnet + clinopyroxene ± hornblende. A specific Cenozoic high-Al TTD (adakite) contains lower Y, Yb and Sc and higher Sr, Sr\u002FY, La\u002FYb and.Zr\u002FSm relative to other TTD types and is interpreted to represent a slab melt under garnet amphibolite to eclogite conditions. High-Al TTD with an adakite-like geochemical character is prevalent in the Archean as the result of a higher geotherm that facilitated slab melting. Cenozoic adakite localities are commonly associated with the subduction of young (<25 Ma), hot oceanic crust, which may provide a slab geotherm (≍9–10°C km\u003Cjats:sup>−1\u003C\u002Fjats:sup>) conducive for slab dehydration melting. Viable alternative or supporting tectonic effects that may enhance slab melting include highly oblique convergence and resultant high shear stresses and incipient subduction into a pristine hot mantle wedge. The minimum\u003Cjats:italic>P–T\u003C\u002Fjats:italic>conditions for slab melting are interpreted to be 22–26 kbar (75–85 km depth) and 750–800°C. This\u003Cjats:italic>P–T\u003C\u002Fjats:italic>regime is framed by the hornblende dehydration, 10°C\u002Fkm, and wet basalt melting curves and coincides with numerous potential slab dehydration reactions, such as tremolite, biotite + quartz, serpentine, talc, Mg-chloritoid, paragonite, clinohumite and talc + phengite. Involvement of overthickened (>50 km) lower continental crust either via direct partial melting or as a contaminant in typical mantle wedge-derived arc magmas has been presented as an alternative to slab melting. However, the intermediate to felsic volcanic and plutonic rocks that involve the lower crust are more highly potassic, enriched in large ion lithophile elements and elevated in Sr isotopic values relative to Cenozoic adakites. Slab-derived adakites, on the other hand, ascend into and react with the mantle wedge and become progressively enriched in MgO, Cr and Ni while retaining their slab melt geochemical signature. Our studies in northern Kamchatka, Russia provide an excellent case example for adakite-mantle interaction and a rare glimpse of trapped slab melt veinlets in Na-metasomatised mantle xenoliths.\u003C\u002Fjats:p>",{"EN":1028},"Petrogenesis of slab-derived trondhjemite–tonalite–dacite\u002Fadakite magmas",{"VOID":1030},"10.1017\u002Fs0263593300006611",[132],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0263593300006611\u002Ftype\u002Fjournal_article",[1034,1053,1074],{"id":1035,"sortIndex":25,"researcher":24,"roles":1036,"affiliations":1037,"properties":1048},"4955f34d-7477-44e9-8f71-6681e4791f4a",[],[1038],{"id":1039,"sortIndex":25,"affiliation":1040,"properties":24},"1df561a0-e92e-4824-b588-804e34263212",{"id":1041,"createTime":1042,"updateTime":1042,"relativeEntities":1043,"slug":1044,"properties":1045,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"5eb3b5ba-848a-49c2-a165-fafe8fdd75fd","2024-09-29T05:19:37.244+00:00",[],"Mark-S-Drummond-Department-of-Geology-University-of-Alabama-at-Birmingham-Birmingham-AL-35294-2160-U-S-A-",{"title":1046},{"EN":1047},"Mark S. Drummond, Department of Geology, University of Alabama at Birmingham, Birmingham, AL 35294-2160, U.S.A.",{"openalex":1049,"title":1051},{"VOID":1050},"A5039162385",{"EN":1052},"Mark S. Drummond",{"id":1054,"sortIndex":53,"researcher":24,"roles":1055,"affiliations":1056,"properties":1067},"15d2fd35-31b9-441a-8390-a2667a4469b9",[],[1057],{"id":1058,"sortIndex":25,"affiliation":1059,"properties":24},"b70c174a-06f9-4a24-8f9d-d63c7678de57",{"id":1060,"createTime":1061,"updateTime":1061,"relativeEntities":1062,"slug":1063,"properties":1064,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"9b7c3672-abcc-4286-b9da-96862a968063","2024-09-29T05:19:37.271+00:00",[],"Pavel-K-Kepezhinskas-Department-of-Geology-University-of-South-Florida-Tampa-FL-33620-5200-U-S-A-",{"title":1065},{"EN":1066},"Pavel K. Kepezhinskas, Department of Geology.University of South Florida, Tampa, FL 33620-5200, U.S.A.",{"openalex":1068,"orcid":1070,"title":1072},{"VOID":1069},"A5086839782",{"VOID":1071},"https:\u002F\u002Forcid.org\u002F0000-0002-3903-6487",{"EN":1073},"Pavel Kepezhinskas",{"id":1075,"sortIndex":193,"researcher":24,"roles":1076,"affiliations":1077,"properties":1088},"e7d19209-19fe-4835-a10c-a2c11786c65b",[],[1078],{"id":1079,"sortIndex":25,"affiliation":1080,"properties":24},"a0cac842-099b-4478-801c-7ca8375380fa",{"id":1081,"createTime":1082,"updateTime":1082,"relativeEntities":1083,"slug":1084,"properties":1085,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"51d3322d-017f-4ab9-baec-6f7bb5113d6e","2024-09-29T05:19:37.260+00:00",[],"Marc-J-Defant-Department-of-Geology-University-of-South-Florida-Tampa-FL-33620-5200-U-S-A-",{"title":1086},{"EN":1087},"Marc J. Defant, Department of Geology, University of South Florida, Tampa, FL 33620-5200, U.S.A.",{"openalex":1089,"title":1091},{"VOID":1090},"A5019971021",{"EN":1092},"Marc J. Defant",{"url":24,"publisher":1094,"properties":1119},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":1095,"slug":10,"properties":1096,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":1102,"manageAffiliations":1103,"indexDatabases":1104,"url":107,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":1097,"issn":1098,"introduce":1099,"eissn":1100,"title":1101},{"VOID":13},{"VOID":15},{"EN":17},{"VOID":19},{"EN":21},[],[],[1105,1112],{"id":68,"indexDatabase":1106,"url":83,"indexYears":24,"academicFieldIds":1111,"indexDatabaseRanking":24},{"id":70,"createTime":71,"updateTime":72,"relativeEntities":1107,"label":1108,"description":1109,"key":79,"publicationTags":1110,"standard":24},[],{"EN":75,"VI":75},{"VI":77,"EN":78},[81,82],[85,86],{"id":88,"indexDatabase":1113,"url":101,"indexYears":102,"academicFieldIds":1118,"indexDatabaseRanking":106},{"id":90,"createTime":91,"updateTime":92,"relativeEntities":1114,"label":1115,"description":1116,"key":98,"publicationTags":1117,"standard":24},[],{"EN":95,"VI":95},{"EN":95,"VI":97},[100],[104,105],{"volume":1120,"pages":1122,"issue":1124},{"VOID":1121},"87",{"VOID":1123},"205-215",{"VOID":189},606,{"total":1125,"publishYear":24,"statisticByYear":1127},{"2012":1128,"2013":1129,"2014":1130,"2015":1131,"2016":1132,"2017":483,"2018":1133,"2019":1134,"2020":1135,"2021":1136,"2022":1137,"2023":861,"2024":860},32,19,21,22,29,35,38,34,33,25,"1996-01-01",1996,[1141,1144,1147,1150,1153,1156,1159,1162,1165,1168,1171,1174,1177,1180,1183,1186,1189,1192,1195,1198,1201,1204,1207,1210,1213,1216,1219,1222,1225,1228,1231,1234,1237,1240,1243,1246,1249,1252,1255,1258,1261,1264,1267,1270,1273,1276,1279,1282,1285,1288,1291,1294,1297,1300,1303,1306,1309,1312,1316,1319,1322,1325,1328,1331,1334,1337,1340,1343,1346,1349,1352,1355,1358,1361,1364,1367,1369,1372,1375,1378,1381,1384,1387,1390,1393,1396,1399,1402,1405,1408,1411,1414,1417,1420,1423,1426,1429,1432,1435,1438,1441,1444,1448,1451,1454,1457,1460,1463,1466,1469,1472,1475,1478,1481,1484],{"id":24,"text":1142,"url":24,"identifiers":1143},"10.1029\u002FJB082i005p00803",{"doi":1142},{"id":24,"text":1145,"url":24,"identifiers":1146},"10.1016\u002F0012-821X(94)90042-6",{"doi":1145},{"id":24,"text":1148,"url":24,"identifiers":1149},"10.1144\u002Fgsjgs.141.5.0803",{"doi":1148},{"id":24,"text":1151,"url":24,"identifiers":1152},"10.1007\u002FBF00321985",{"doi":1151},{"id":24,"text":1154,"url":24,"identifiers":1155},"10.1029\u002FJB091iB06p05913",{"doi":1154},{"id":24,"text":1157,"url":24,"identifiers":1158},"10.1130\u002F0016-7606(1993)105\u003C0715:LBACOS>2.3.CO;2",{"doi":1157},{"id":24,"text":1160,"url":24,"identifiers":1161},"10.1126\u002Fscience.268.5212.858",{"doi":1160},{"id":24,"text":1163,"url":24,"identifiers":1164},"10.1098\u002Frsta.1981.0105",{"doi":1163},{"id":24,"text":1166,"url":24,"identifiers":1167},"10.1029\u002FTC009i005p01197",{"doi":1166},{"id":24,"text":1169,"url":24,"identifiers":1170},"10.1093\u002Fpetrology\u002F28.5.921",{"doi":1169},{"id":24,"text":1172,"url":24,"identifiers":1173},"10.1029\u002FTC003i004p00429",{"doi":1172},{"id":24,"text":1175,"url":24,"identifiers":1176},"Ringwood, 1975, Composition and petrology of the earth's mantle",{},{"id":24,"text":1178,"url":24,"identifiers":1179},"10.1093\u002Fpetrology\u002F30.6.1351",{"doi":1178},{"id":24,"text":1181,"url":24,"identifiers":1182},"Condie, 1981, Archean greenstone belts",{},{"id":24,"text":1184,"url":24,"identifiers":1185},"10.1086\u002F628690",{"doi":1184},{"id":24,"text":1187,"url":24,"identifiers":1188},"10.1016\u002F0031-9201(84)90030-X",{"doi":1187},{"id":24,"text":1190,"url":24,"identifiers":1191},"10.1029\u002FJB080i032p04405",{"doi":1190},{"id":24,"text":1193,"url":24,"identifiers":1194},"10.1007\u002FBF00371551",{"doi":1193},{"id":24,"text":1196,"url":24,"identifiers":1197},"10.1007\u002FBF01166961",{"doi":1196},{"id":24,"text":1199,"url":24,"identifiers":1200},"10.1038\u002F362144a0",{"doi":1199},{"id":24,"text":1202,"url":24,"identifiers":1203},"10.1007\u002FBF01829365",{"doi":1202},{"id":24,"text":1205,"url":24,"identifiers":1206},"10.1093\u002Fpetrology\u002F24.1.1",{"doi":1205},{"id":24,"text":1208,"url":24,"identifiers":1209},"10.1016\u002F0012-821X(83)90094-8",{"doi":1208},{"id":24,"text":1211,"url":24,"identifiers":1212},"Rapp R. 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A. & Peate D. W. 1995. Tectonic implications of the composition of volcanic arc magmas. In Wetherill G. W. , Albee A. L. & Burke K. C. 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191",{},{"id":24,"text":1304,"url":24,"identifiers":1305},"10.1093\u002Fpetrology\u002F32.2.365",{"doi":1304},{"id":24,"text":1307,"url":24,"identifiers":1308},"10.2475\u002Fajs.295.7.875",{"doi":1307},{"id":24,"text":1310,"url":24,"identifiers":1311},"10.1007\u002FBF00307273",{"doi":1310},{"id":24,"text":1313,"url":24,"identifiers":1314},"Bowring, 1990, Origin of the earth, 319, 10.1093\u002Foso\u002F9780195066197.003.0018",{"doi":1315},"10.1093\u002Foso\u002F9780195066197.003.0018",{"id":24,"text":1317,"url":24,"identifiers":1318},"10.1007\u002FBF00286939",{"doi":1317},{"id":24,"text":1320,"url":24,"identifiers":1321},"10.1007\u002FBF00311004",{"doi":1320},{"id":24,"text":1323,"url":24,"identifiers":1324},"10.1007\u002FBF01820584",{"doi":1323},{"id":24,"text":1326,"url":24,"identifiers":1327},"10.1029\u002F95JB00861",{"doi":1326},{"id":24,"text":1329,"url":24,"identifiers":1330},"10.1016\u002F0377-0273(78)90032-X",{"doi":1329},{"id":24,"text":1332,"url":24,"identifiers":1333},"Cande, 1989, Magnetic lineations of the world's ocean 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1995, The eclogitized pillows of the Betic Ophiolitic Association: relics of the Tethys Ocean floor incorporated in the Alpine chain after subduction, TERRA REV, 7, 31",{},{"id":24,"text":1403,"url":24,"identifiers":1404},"10.1016\u002F0301-9268(91)90092-O",{"doi":1403},{"id":24,"text":1406,"url":24,"identifiers":1407},"10.1007\u002FBF00311184",{"doi":1406},{"id":24,"text":1409,"url":24,"identifiers":1410},"Rushmer, 1994, Trace element behavior during slab melting: experimental evidence, EOS, TRANS AM GEOPHYS UNION, 75, 746",{},{"id":24,"text":1412,"url":24,"identifiers":1413},"10.1130\u002F0091-7613(1993)021\u003C1007:IOSATG>2.3.CO;2",{"doi":1412},{"id":24,"text":1415,"url":24,"identifiers":1416},"10.1180\u002Fminmag.1988.052.364.01",{"doi":1415},{"id":24,"text":1418,"url":24,"identifiers":1419},"10.1007\u002FBF00310465",{"doi":1418},{"id":24,"text":1421,"url":24,"identifiers":1422},"10.1111\u002Fj.1525-1314.1988.tb00431.x",{"doi":1421},{"id":24,"text":1424,"url":24,"identifiers":1425},"10.1007\u002F978-1-4684-7335-3_4",{"doi":1424},{"id":24,"text":1427,"url":24,"identifiers":1428},"Tatsumi, 1995, Subduction zone magmatism",{},{"id":24,"text":1430,"url":24,"identifiers":1431},"10.1016\u002F0012-821X(82)90008-5",{"doi":1430},{"id":24,"text":1433,"url":24,"identifiers":1434},"10.1016\u002F0377-0273(86)90049-1",{"doi":1433},{"id":24,"text":1436,"url":24,"identifiers":1437},"10.1029\u002F94JB00458",{"doi":1436},{"id":24,"text":1439,"url":24,"identifiers":1440},"10.1007\u002F978-94-011-6489-4",{"doi":1439},{"id":24,"text":1442,"url":24,"identifiers":1443},"10.1016\u002F0016-7037(95)00038-2",{"doi":1442},{"id":24,"text":1445,"url":24,"identifiers":1446},"Winther, 1991, Experimental melting of hydrous low-K tholeiite: evidence on the origin of Archaean cratons, BULL GEOL SOC DENMARK, 39, 213, 10.37570\u002Fbgsd-1991-39-10",{"doi":1447},"10.37570\u002Fbgsd-1991-39-10",{"id":24,"text":1449,"url":24,"identifiers":1450},"10.1007\u002FBF00320972",{"doi":1449},{"id":24,"text":1452,"url":24,"identifiers":1453},"10.1130\u002F0016-7606(1982)93\u003C468:SPATEP>2.0.CO;2",{"doi":1452},{"id":24,"text":1455,"url":24,"identifiers":1456},"10.1093\u002Fpetrology\u002F35.1.163",{"doi":1455},{"id":24,"text":1458,"url":24,"identifiers":1459},"10.1130\u002F0016-7606(1995)107\u003C0505:MAITWA>2.3.CO;2",{"doi":1458},{"id":24,"text":1461,"url":24,"identifiers":1462},"10.1016\u002F0016-7037(89)90096-3",{"doi":1461},{"id":24,"text":1464,"url":24,"identifiers":1465},"10.1093\u002Fpetrology\u002F36.4.891",{"doi":1464},{"id":24,"text":1467,"url":24,"identifiers":1468},"10.1080\u002F00206818909465876",{"doi":1467},{"id":24,"text":1470,"url":24,"identifiers":1471},"Kepezhinskas P. K. , McDermott F. , Defant M. J. , Hochstaedter A. , Drummond M. S. , Hawkesworth C. , Koloskov A. , Maury R. C. & Bellon H. Trace element and Sr–Nd–Pb isotope geochemistry of the Kamchatka volcanic arc, Russia. GEOCHIM COSMOCHIM ACTA, in press.",{},{"id":24,"text":1473,"url":24,"identifiers":1474},"10.1029\u002F95JB00913",{"doi":1473},{"id":24,"text":1476,"url":24,"identifiers":1477},"10.1130\u002F0016-7606(1976)87\u003C189:TTBTOS>2.0.CO;2",{"doi":1476},{"id":24,"text":1479,"url":24,"identifiers":1480},"Taylor, 1985, The continental crust: its composition and evolution",{},{"id":24,"text":1482,"url":24,"identifiers":1483},"10.1093\u002Fpetrology\u002F35.3.577",{"doi":1482},{"id":24,"text":1485,"url":24,"identifiers":1486},"10.1098\u002Frsta.1981.0122",{"doi":1485},{"id":1488,"createTime":1489,"updateTime":1489,"relativeEntities":1490,"slug":1491,"properties":1492,"entityType":127,"verifyStatus":128,"verifyTime":1502,"verifyNote":130,"syncStatus":23,"languages":1503,"translateLanguages":24,"viewCount":25,"primaryUrl":1504,"fullTextUrl":24,"authors":1505,"publicationType":156,"publisherRelationship":1527,"citationCount":1558,"citationInfo":1559,"publishDate":1138,"publishYear":1139,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":24,"openAccess":24,"references":1563,"isForceReanalyzing":401},"9a0c77da-ada8-4704-8f36-d84d2de05f52","2024-10-02T03:31:59.932+00:00",[],"Lachlan-Fold-Belt-granitoids-products-of-three-component-mixing",{"keywords":1493,"openalex":1494,"abstract":1496,"title":1498,"doi":1500},{},{"VOID":1495},"W4251993829",{"EN":1497},"\u003Cjats:title>ABSTRACT:\u003C\u002Fjats:title>\u003Cjats:p>The paradox of Lachlan Fold Belt (LFB) granitoids is that although contrasted chemical types (S- and I-types) imply melting of distinct crustal sources, the simple Nd–Sr–Pb–O isotopic arrays indicate a continuum, suggesting mixing of magmatic components. The paradox is resolved by the recognition that the previously inferred, isotopically primitive end-member is itself a crust-mantle mix, so that three general source components, mantle, lower crust and middle crust, comprise the granitoids. Based on Nd isotopic evidence, mantle-derived basaltic magmas melted and mixed with Neoproterozoic-Cambrian, arc-backarc-type material to produce primitive I-type, parental granitoid magmas in the lower–middle crust. Ordovician metasediment, locally underthrust to mid-crustal levels, was remobilised under the elevated geotherms and is most clearly recognised as diatexite in the Cooma complex, but it also exists as gneissic enclaves in S-type granites. The diatexite mixed with the hybrid I-type magmas to produce the parental S-type magmas. Unique parent magma compositions of individual granite suites reflect variations within any or all of the three major source components, or between the mixing proportions. For example, chemical tie-lines between Cooma diatexite and mafic I-type Jindabyne suite magma encompass almost all mafic S-type granites of the vast Bullenbalong supersuite, consistently in the proportion Jindabyne: Cooma, 30:70. The modelling shows that LFB S-type magmas are heavily contaminated I-type magmas, produced by large-scale mixing of hot I-type material with lower temperature diatexite in the middle crust. The model implies a genetic link between migmatite and pluton-scale, crustally derived (S-type) granites.\u003C\u002Fjats:p>\u003Cjats:p>Given the chemical and isotopic contrasts of the crustally derived source components, and their typically unequal proportions in the magmas, it is not surprising that the LFB granitoids are so distinctive and have been categorised as S- and I-type. The sublinear chemical trends of the granitoid suites are considered to be secondary effects associated with crystal fractionation of unique parental magmas that were formed by three-component mixing. The model obviates the necessity for multiple underplating events and Proterozoic continental basement, in accordance with the observed tectonostratigraphy of the Lachlan Fold Belt.\u003C\u002Fjats:p>",{"EN":1499},"Lachlan Fold Belt granitoids: products of three-component mixing",{"VOID":1501},"10.1017\u002Fs0263593300006581","2024-10-02T03:31:59.931+00:00",[132],"https:\u002F\u002Fwww.cambridge.org\u002Fcore\u002Fproduct\u002Fidentifier\u002FS0263593300006581\u002Ftype\u002Fjournal_article",[1506],{"id":1507,"sortIndex":25,"researcher":24,"roles":1508,"affiliations":1509,"properties":1520},"43144b23-1f67-45a7-a1ac-49fe45d22689",[],[1510],{"id":1511,"sortIndex":25,"affiliation":1512,"properties":24},"204e38cc-5be8-4578-8f8d-86d9a3b779c0",{"id":1513,"createTime":1514,"updateTime":1514,"relativeEntities":1515,"slug":1516,"properties":1517,"entityType":52,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"syncStatus":23,"languages":24,"translateLanguages":24,"viewCount":25},"e7d5788e-5850-49f4-af91-33b054a2ebe9","2024-10-02T03:31:59.949+00:00",[],"W-J-Collins-Department-of-Geology-University-of-Newcastle-Newcastle-NSW-2308-Australia-",{"title":1518},{"EN":1519},"W. J. Collins, Department of Geology, University of Newcastle, Newcastle, NSW, 2308, Australia.",{"openalex":1521,"orcid":1523,"title":1525},{"VOID":1522},"A5101813809",{"VOID":1524},"https:\u002F\u002Forcid.org\u002F0000-0003-3982-6873",{"EN":1526},"William J. 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