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Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks

dc.contributor.authorLi, W.
dc.contributor.authorLi, X.
dc.contributor.authorLi, Zheng-Xiang
dc.contributor.authorLou, F.
dc.date.accessioned2017-01-30T15:31:44Z
dc.date.available2017-01-30T15:31:44Z
dc.date.created2014-10-08T06:00:44Z
dc.date.issued2008
dc.identifier.citationLi, W. and Li, X. and Li, Z. and Lou, F. 2008. Obduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks. Gondwana Research.. 13 (3): pp. 288-301.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/47181
dc.publisherElsevier Science BV
dc.titleObduction-type granites within the NE Jiangxi Ophiolite: Implications for the final amalgamation between the Yangtze and Cathaysia Blocks
dc.typeJournal Article
dcterms.source.volume13
dcterms.source.number3
dcterms.source.startPage288
dcterms.source.endPage301
dcterms.source.issn1342937X
dcterms.source.titleGondwana Research.
curtin.departmentDepartment of Applied Geology
curtin.accessStatusFulltext not available


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