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Article: Geodynamic settings and tectonic model of skarn gold deposits in China: An overview

TitleGeodynamic settings and tectonic model of skarn gold deposits in China: An overview
Authors
KeywordsChina
Cmf Model
Continental Collision
Metallogenic Timing
Orogenesis
Skarn Gold Deposit
Tectonic Provinces
Issue Date2007
PublisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/oregeorev
Citation
Ore Geology Reviews, 2007, v. 31 n. 1-4, p. 139-169 How to Cite?
AbstractSeventy skarn-type gold deposits, including 1 super-large, 19 large and 24 medium-sized, are known from different geotectonic units of China. They contain a total resource of approximately 1000 t of gold (625 t in South China), and account for 20% of China's gold reserves. These skarn deposits are sited in collisional orogenic belts, fault-controlled magmatic belts and reactivated cratonic margins. All of the Chinese skarn gold provinces were affected by Phanerozoic collisional orogenesis. The timing of the metallogenic events and the spatial-temporal distribution of the Chinese skarn gold deposits indicates that they were formed during ore-forming processes linked to the transition from shortening to extension in the geodynamic evolution of a collision orogen, and not to subduction systems as is commonly advocated for porphyry copper systems around the Pacific Rim. © 2006 Elsevier B.V. All rights reserved.
Persistent Identifierhttp://hdl.handle.net/10722/92334
ISSN
2015 Impact Factor: 3.819
2015 SCImago Journal Rankings: 1.753
ISI Accession Number ID
References

 

DC FieldValueLanguage
dc.contributor.authorChen, Y-Jen_HK
dc.contributor.authorChen, H-Yen_HK
dc.contributor.authorZaw, Ken_HK
dc.contributor.authorPirajno, Fen_HK
dc.contributor.authorZhang, Z-Jen_HK
dc.date.accessioned2010-09-17T10:42:58Z-
dc.date.available2010-09-17T10:42:58Z-
dc.date.issued2007en_HK
dc.identifier.citationOre Geology Reviews, 2007, v. 31 n. 1-4, p. 139-169en_HK
dc.identifier.issn0169-1368en_HK
dc.identifier.urihttp://hdl.handle.net/10722/92334-
dc.description.abstractSeventy skarn-type gold deposits, including 1 super-large, 19 large and 24 medium-sized, are known from different geotectonic units of China. They contain a total resource of approximately 1000 t of gold (625 t in South China), and account for 20% of China's gold reserves. These skarn deposits are sited in collisional orogenic belts, fault-controlled magmatic belts and reactivated cratonic margins. All of the Chinese skarn gold provinces were affected by Phanerozoic collisional orogenesis. The timing of the metallogenic events and the spatial-temporal distribution of the Chinese skarn gold deposits indicates that they were formed during ore-forming processes linked to the transition from shortening to extension in the geodynamic evolution of a collision orogen, and not to subduction systems as is commonly advocated for porphyry copper systems around the Pacific Rim. © 2006 Elsevier B.V. All rights reserved.en_HK
dc.languageengen_HK
dc.publisherElsevier BV. The Journal's web site is located at http://www.elsevier.com/locate/oregeoreven_HK
dc.relation.ispartofOre Geology Reviewsen_HK
dc.subjectChinaen_HK
dc.subjectCmf Modelen_HK
dc.subjectContinental Collisionen_HK
dc.subjectMetallogenic Timingen_HK
dc.subjectOrogenesisen_HK
dc.subjectSkarn Gold Depositen_HK
dc.subjectTectonic Provincesen_HK
dc.titleGeodynamic settings and tectonic model of skarn gold deposits in China: An overviewen_HK
dc.typeArticleen_HK
dc.identifier.emailChen, Y:ychenc@hkucc.hku.hken_HK
dc.identifier.authorityChen, Y=rp1318en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.oregeorev.2005.01.001en_HK
dc.identifier.scopuseid_2-s2.0-33947174641en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-33947174641&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume31en_HK
dc.identifier.issue1-4en_HK
dc.identifier.spage139en_HK
dc.identifier.epage169en_HK
dc.identifier.isiWOS:000245847500006-

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