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Article: Shoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry
Title | Shoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry |
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Authors | |
Keywords | Element geochemistry Guangxi Petrology Shoshonitic rocks |
Issue Date | 2000 |
Publisher | Science 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? |
Abstract | A 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 Identifier | http://hdl.handle.net/10722/72619 |
ISSN | 2016 Impact Factor: 1.649 |
ISI Accession Number ID | |
References |
DC Field | Value | Language |
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dc.contributor.author | Li, X | en_HK |
dc.contributor.author | Zhou, H | en_HK |
dc.contributor.author | Liu, Y | en_HK |
dc.contributor.author | Lee, CY | en_HK |
dc.contributor.author | Sun, M | en_HK |
dc.contributor.author | Chen, C | en_HK |
dc.date.accessioned | 2010-09-06T06:43:32Z | - |
dc.date.available | 2010-09-06T06:43:32Z | - |
dc.date.issued | 2000 | en_HK |
dc.identifier.citation | Chinese Science Bulletin, 2000, v. 45 n. 7, p. 653-659 | en_HK |
dc.identifier.issn | 1001-6538 | en_HK |
dc.identifier.uri | http://hdl.handle.net/10722/72619 | - |
dc.description.abstract | A 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.language | eng | en_HK |
dc.publisher | Science China Press. The Journal's web site is located at http://www.springerlink.com/content/1001-6538/ | en_HK |
dc.relation.ispartof | Chinese Science Bulletin | en_HK |
dc.subject | Element geochemistry | en_HK |
dc.subject | Guangxi | en_HK |
dc.subject | Petrology | en_HK |
dc.subject | Shoshonitic rocks | en_HK |
dc.title | Shoshonitic intrusive suite in SE Guangxi: Petrology and geochemistry | en_HK |
dc.type | Article | en_HK |
dc.identifier.openurl | http://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.email | Sun, M:minsun@hku.hk | en_HK |
dc.identifier.authority | Sun, M=rp00780 | en_HK |
dc.description.nature | link_to_subscribed_fulltext | - |
dc.identifier.scopus | eid_2-s2.0-0034484774 | en_HK |
dc.identifier.hkuros | 58003 | en_HK |
dc.relation.references | http://www.scopus.com/mlt/select.url?eid=2-s2.0-0034484774&selection=ref&src=s&origin=recordpage | en_HK |
dc.identifier.volume | 45 | en_HK |
dc.identifier.issue | 7 | en_HK |
dc.identifier.spage | 653 | en_HK |
dc.identifier.epage | 659 | en_HK |
dc.identifier.isi | WOS:000086083700015 | - |
dc.publisher.place | China | en_HK |
dc.identifier.scopusauthorid | Li, X=7501704180 | en_HK |
dc.identifier.scopusauthorid | Zhou, H=7404742065 | en_HK |
dc.identifier.scopusauthorid | Liu, Y=26651938100 | en_HK |
dc.identifier.scopusauthorid | Lee, CY=7410158730 | en_HK |
dc.identifier.scopusauthorid | Sun, M=25932315800 | en_HK |
dc.identifier.scopusauthorid | Chen, C=7501967170 | en_HK |
dc.identifier.issnl | 1001-6538 | - |