Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/104586
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dc.contributor.authorDai, J.en
dc.contributor.authorWang, C.en
dc.contributor.authorPolat, A.en
dc.contributor.authorSantosh, M.en
dc.contributor.authorLi, Y.en
dc.contributor.authorGe, Y.en
dc.date.issued2013en
dc.identifier.citationLithos, 2013; 172-173:1-16en
dc.identifier.issn0024-4937en
dc.identifier.issn1872-6143en
dc.identifier.urihttp://hdl.handle.net/2440/104586-
dc.description.abstractAbstract not availableen
dc.description.statementofresponsibilityJingen Dai, Chengshan Wang, Ali Polat, M. Santosh, Yalin Li, Yukui Geen
dc.language.isoenen
dc.publisherElsevieren
dc.rights© 2013 Elsevier B.V. All rights reserved.en
dc.subjectXigaze ophiolite; supra-subduction zone; geochemistry; zircon U–Pb geochronology; slab rollbacken
dc.titleRapid forearc spreading between 130 and 120Ma: evidence from geochronology and geochemistry of the Xigaze ophiolite, southern Tibeten
dc.typeJournal articleen
dc.identifier.rmid0030044531en
dc.identifier.doi10.1016/j.lithos.2013.03.011en
dc.identifier.pubid235397-
pubs.library.collectionGeology & Geophysics publicationsen
pubs.library.teamDS11en
pubs.verification-statusVerifieden
pubs.publication-statusPublisheden
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]en
Appears in Collections:Geology & Geophysics publications

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