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Article: Shoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry

TitleShoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry
Authors
KeywordsElement geochemistry
Guangxi
Petrology
Shoshonitic rocks
Issue Date2000
PublisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/
Citation
Chinese Science Bulletin, 2000, v. 45 n. 7, p. 653-659 How to Cite?
AbstractA NE-direction Mesozoic shoshonitic intrusive suite in SE Guangxi has been identified in terms of geological, petrological and geochemical investigations. The shoshonitic intrusives are characterized by enrichment of LILE, HFSE and LREE and no obvious Nb-Ta depletion, similar to those potassic rocks formed in within-plate and rifting environments. Unlike most shoshonitic rocks forming in arc settings, the SE Guangxi shoshonitic intrusives were likely generated during regional lithosphere extension induced by upwelling of asthenosphere mantle.
Persistent Identifierhttp://hdl.handle.net/10722/72619
ISSN
2015 Impact Factor: 1.789
References

 

DC FieldValueLanguage
dc.contributor.authorLi, Xen_HK
dc.contributor.authorZhou, Hen_HK
dc.contributor.authorLiu, Yen_HK
dc.contributor.authorLee, CYen_HK
dc.contributor.authorSun, Men_HK
dc.contributor.authorChen, Cen_HK
dc.date.accessioned2010-09-06T06:43:32Z-
dc.date.available2010-09-06T06:43:32Z-
dc.date.issued2000en_HK
dc.identifier.citationChinese Science Bulletin, 2000, v. 45 n. 7, p. 653-659en_HK
dc.identifier.issn1001-6538en_HK
dc.identifier.urihttp://hdl.handle.net/10722/72619-
dc.description.abstractA NE-direction Mesozoic shoshonitic intrusive suite in SE Guangxi has been identified in terms of geological, petrological and geochemical investigations. The shoshonitic intrusives are characterized by enrichment of LILE, HFSE and LREE and no obvious Nb-Ta depletion, similar to those potassic rocks formed in within-plate and rifting environments. Unlike most shoshonitic rocks forming in arc settings, the SE Guangxi shoshonitic intrusives were likely generated during regional lithosphere extension induced by upwelling of asthenosphere mantle.en_HK
dc.languageengen_HK
dc.publisherScience China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/en_HK
dc.relation.ispartofChinese Science Bulletinen_HK
dc.subjectElement geochemistryen_HK
dc.subjectGuangxien_HK
dc.subjectPetrologyen_HK
dc.subjectShoshonitic rocksen_HK
dc.titleShoshonitic intrusive suite in SE Guangxi: Petrology and geochemistryen_HK
dc.typeArticleen_HK
dc.identifier.openurlhttp://library.hku.hk:4550/resserv?sid=HKU:IR&issn=1001-6538&volume=45 &issue=7&spage=653&epage=659&date=2000&atitle=Shoshonitic+intrusive+suite+in+SE+Guangxi:+Petrology+and+geochemistry.en_HK
dc.identifier.emailSun, M:minsun@hku.hken_HK
dc.identifier.authoritySun, M=rp00780en_HK
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.scopuseid_2-s2.0-0034484774en_HK
dc.identifier.hkuros58003en_HK
dc.relation.referenceshttp://www.scopus.com/mlt/select.url?eid=2-s2.0-0034484774&selection=ref&src=s&origin=recordpageen_HK
dc.identifier.volume45en_HK
dc.identifier.issue7en_HK
dc.identifier.spage653en_HK
dc.identifier.epage659en_HK
dc.publisher.placeChinaen_HK
dc.identifier.scopusauthoridLi, X=7501704180en_HK
dc.identifier.scopusauthoridZhou, H=7404742065en_HK
dc.identifier.scopusauthoridLiu, Y=26651938100en_HK
dc.identifier.scopusauthoridLee, CY=7410158730en_HK
dc.identifier.scopusauthoridSun, M=25932315800en_HK
dc.identifier.scopusauthoridChen, C=7501967170en_HK

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