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Article: The Zhaotong native copper deposit associated with the Permian Emeishan flood basalts, Yunnan, Southwest China

TitleThe Zhaotong native copper deposit associated with the Permian Emeishan flood basalts, Yunnan, Southwest China
Authors
Issue Date2006
PublisherTaylor & Francis Inc. The Journal's web site is located at http://www.tandf.co.uk/journals/TIGR
Citation
International Geology Review, 2006, v. 48 n. 8, p. 742-753 How to Cite?
AbstractThe Zhaotong native copper deposit in Yunnan, Southwest China, is associated with the upper Middle Permian Emeishan flood basalts and is mainly hosted in the upper part of the Emeishan volcanic succession. Native copper mainly appears as disseminations in basaltic tuffs, and vesicular and brecciated tops of subaerial lava flows. Sheets of native copper up to 30 × 10 × 0.2 cm have also been found along fractures within the volcanic breccias. The native copper is associated with bitumen, zeolite, quartz, and calcite, typical of a low-temperature (100-150°C) hydrothermal alteration assemblage. The ore grades vary from ∼0.1 to 20 wt% Cu. Copper was likely a result of organic-inorganic interactions under conditions of the paucity of reduced S. Copyright © 2006 by V.H. Winston & Son, Inc. All rights reserved.
Persistent Identifierhttp://hdl.handle.net/10722/72555
ISSN
2015 Impact Factor: 2.365
2015 SCImago Journal Rankings: 1.248
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorWang, CYen_HK
dc.contributor.authorZhou, MFen_HK
dc.contributor.authorQi, Len_HK
dc.contributor.authorHou, Sen_HK
dc.contributor.authorGao, Hen_HK
dc.contributor.authorZhang, Zen_HK
dc.contributor.authorMalpas, Jen_HK
dc.date.accessioned2010-09-06T06:42:56Z-
dc.date.available2010-09-06T06:42:56Z-
dc.date.issued2006en_HK
dc.identifier.citationInternational Geology Review, 2006, v. 48 n. 8, p. 742-753en_HK
dc.identifier.issn0020-6814en_HK
dc.identifier.urihttp://hdl.handle.net/10722/72555-
dc.description.abstractThe Zhaotong native copper deposit in Yunnan, Southwest China, is associated with the upper Middle Permian Emeishan flood basalts and is mainly hosted in the upper part of the Emeishan volcanic succession. Native copper mainly appears as disseminations in basaltic tuffs, and vesicular and brecciated tops of subaerial lava flows. Sheets of native copper up to 30 × 10 × 0.2 cm have also been found along fractures within the volcanic breccias. The native copper is associated with bitumen, zeolite, quartz, and calcite, typical of a low-temperature (100-150°C) hydrothermal alteration assemblage. The ore grades vary from ∼0.1 to 20 wt% Cu. Copper was likely a result of organic-inorganic interactions under conditions of the paucity of reduced S. Copyright © 2006 by V.H. Winston & Son, Inc. All rights reserved.en_HK
dc.languageengen_HK
dc.publisherTaylor & Francis Inc. The Journal's web site is located at http://www.tandf.co.uk/journals/TIGRen_HK
dc.relation.ispartofInternational Geology Reviewen_HK
dc.titleThe Zhaotong native copper deposit associated with the Permian Emeishan flood basalts, Yunnan, Southwest Chinaen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=0020-6814&volume=48&issue=8&spage=742&epage=753&date=2006&atitle=The+Zhaotong+native+copper+deposit+associated+with+the+Permian+Emeishan+flood+basalts,+Yunnan,+Southwest+Chinaen_HK
dc.identifier.emailZhou, MF: mfzhou@hkucc.hku.hken_HK
dc.identifier.emailMalpas, J: jgmalpas@hku.hken_HK
dc.identifier.authorityZhou, MF=rp00844en_HK
dc.identifier.authorityMalpas, J=rp00059en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.2747/0020-6814.48.8.742-
dc.identifier.scopuseid_2-s2.0-33747161958en_HK
dc.identifier.hkuros111434en_HK
dc.identifier.hkuros167282-
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33747161958&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume48en_HK
dc.identifier.issue8en_HK
dc.identifier.spage742en_HK
dc.identifier.epage753en_HK
dc.identifier.isiWOS:000239416400004-
dc.publisher.placeUnited Statesen_HK
dc.identifier.scopusauthoridWang, CY=35849436700en_HK
dc.identifier.scopusauthoridZhou, MF=7403506005en_HK
dc.identifier.scopusauthoridQi, L=7202149924en_HK
dc.identifier.scopusauthoridHou, S=15831580600en_HK
dc.identifier.scopusauthoridGao, H=14066136800en_HK
dc.identifier.scopusauthoridZhang, Z=9238377100en_HK
dc.identifier.scopusauthoridMalpas, J=7006136845en_HK
dc.customcontrol.immutablesml 130308-

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