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Article: Geochemistry and petrogenesis of the Yishak Volcanic Sequence, Kudi ophiolite, West Kunlun (NW China): Implications for the magmatic evolution in a subduction zone environment

TitleGeochemistry and petrogenesis of the Yishak Volcanic Sequence, Kudi ophiolite, West Kunlun (NW China): Implications for the magmatic evolution in a subduction zone environment
Authors
KeywordsEarth sciences
Geology mines and mining industry
Issue Date2005
PublisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00410/index.htm
Citation
Contributions To Mineralogy And Petrology, 2005, v. 150 n. 2, p. 195-211 How to Cite?
AbstractThe Yishak Volcanic Series (YVS) is part of the Late Cambrian Kudi ophiolite in the western Kunlun Mountains, NW China, which marks the oldest suture zone in the Tibetan Plateau. The YVS is a well-preserved sequence comprising five conformable units (A to E) of basalts to andesites, with mafic dykes in Units A to D. These rocks are sequentially characterized upward by geochemical features of N-MORB (Unit A), E-MORB (Unit B), island-arc basalt (Unit C), BABB (Unit D and mafic dykes) and boninite series rocks (Unit E), reflecting complex interactions among various source components. The evolution of magma compositions from MORB-dominated to boninite series rocks clearly indicates temporally increasing subduction signatures, which, in combination with the extensional tectonic background, suggests that the Kudi ophiolite most likely formed in a spontaneous nucleation of subduction zone. © Springer-Verlag 2005.
Persistent Identifierhttp://hdl.handle.net/10722/48579
ISSN
2015 Impact Factor: 3.218
2015 SCImago Journal Rankings: 2.582
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorYuan, Cen_HK
dc.contributor.authorSun, Men_HK
dc.contributor.authorZhou, MFen_HK
dc.contributor.authorXiao, Wen_HK
dc.contributor.authorZhou, Hen_HK
dc.date.accessioned2008-05-22T04:17:46Z-
dc.date.available2008-05-22T04:17:46Z-
dc.date.issued2005en_HK
dc.identifier.citationContributions To Mineralogy And Petrology, 2005, v. 150 n. 2, p. 195-211en_HK
dc.identifier.issn0010-7999en_HK
dc.identifier.urihttp://hdl.handle.net/10722/48579-
dc.description.abstractThe Yishak Volcanic Series (YVS) is part of the Late Cambrian Kudi ophiolite in the western Kunlun Mountains, NW China, which marks the oldest suture zone in the Tibetan Plateau. The YVS is a well-preserved sequence comprising five conformable units (A to E) of basalts to andesites, with mafic dykes in Units A to D. These rocks are sequentially characterized upward by geochemical features of N-MORB (Unit A), E-MORB (Unit B), island-arc basalt (Unit C), BABB (Unit D and mafic dykes) and boninite series rocks (Unit E), reflecting complex interactions among various source components. The evolution of magma compositions from MORB-dominated to boninite series rocks clearly indicates temporally increasing subduction signatures, which, in combination with the extensional tectonic background, suggests that the Kudi ophiolite most likely formed in a spontaneous nucleation of subduction zone. © Springer-Verlag 2005.en_HK
dc.format.extent223018 bytes-
dc.format.extent3712 bytes-
dc.format.mimetypeapplication/pdf-
dc.format.mimetypetext/plain-
dc.languageengen_HK
dc.publisherSpringer Verlag. The Journal's web site is located at http://link.springer.de/link/service/journals/00410/index.htmen_HK
dc.relation.ispartofContributions to Mineralogy and Petrologyen_HK
dc.rightsThe original publication is available at www.springerlink.comen_HK
dc.rightsCreative Commons: Attribution 3.0 Hong Kong License-
dc.subjectEarth sciencesen_HK
dc.subjectGeology mines and mining industryen_HK
dc.titleGeochemistry and petrogenesis of the Yishak Volcanic Sequence, Kudi ophiolite, West Kunlun (NW China): Implications for the magmatic evolution in a subduction zone environmenten_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0010-7999&volume=150&issue=2&spage=195&epage=211&date=2005&atitle=Geochemistry+and+petrogenesis+of+the+Yishak+Volcanic+Sequence,+Kudi+ophiolite,+West+Kunlun+(NW+China):+implications+for+the+magmatic+evolution+in+a+subduction+zone+environmenten_HK
dc.identifier.emailYuan, C: yuanchao@HKUCC-COM.hku.hken_HK
dc.identifier.emailSun, M: minsun@hku.hken_HK
dc.identifier.emailZhou, MF: mfzhou@hkucc.hku.hk-
dc.identifier.authoritySun, M=rp00780en_HK
dc.identifier.authorityZhou, MF=rp00844en_HK
dc.description.naturepostprinten_HK
dc.identifier.doi10.1007/s00410-005-0012-0en_HK
dc.identifier.scopuseid_2-s2.0-27244458935en_HK
dc.identifier.hkuros109770-
dc.identifier.hkuros120051-
dc.identifier.hkuros127642-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-27244458935&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume150en_HK
dc.identifier.issue2en_HK
dc.identifier.spage195en_HK
dc.identifier.epage211en_HK
dc.identifier.isiWOS:000232401100005-
dc.publisher.placeGermanyen_HK
dc.identifier.scopusauthoridYuan, C=35241599200en_HK
dc.identifier.scopusauthoridSun, M=25932315800en_HK
dc.identifier.scopusauthoridZhou, MF=7403506005en_HK
dc.identifier.scopusauthoridXiao, W=7202456615en_HK
dc.identifier.scopusauthoridZhou, H=7404741996en_HK

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