Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/104586
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dc.contributor.authorDai, J.-
dc.contributor.authorWang, C.-
dc.contributor.authorPolat, A.-
dc.contributor.authorSantosh, M.-
dc.contributor.authorLi, Y.-
dc.contributor.authorGe, Y.-
dc.date.issued2013-
dc.identifier.citationLithos, 2013; 172-173:1-16-
dc.identifier.issn0024-4937-
dc.identifier.issn1872-6143-
dc.identifier.urihttp://hdl.handle.net/2440/104586-
dc.description.abstractAbstract not available-
dc.description.statementofresponsibilityJingen Dai, Chengshan Wang, Ali Polat, M. Santosh, Yalin Li, Yukui Ge-
dc.language.isoen-
dc.publisherElsevier-
dc.rights© 2013 Elsevier B.V. All rights reserved.-
dc.source.urihttp://dx.doi.org/10.1016/j.lithos.2013.03.011-
dc.subjectXigaze ophiolite; supra-subduction zone; geochemistry; zircon U–Pb geochronology; slab rollback-
dc.titleRapid forearc spreading between 130 and 120Ma: evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibet-
dc.typeJournal article-
dc.identifier.doi10.1016/j.lithos.2013.03.011-
pubs.publication-statusPublished-
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]-
Appears in Collections:Aurora harvest 3
Geology & Geophysics publications

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