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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/104515
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dc.contributor.authorZhang, L.-
dc.contributor.authorWang, Q.-
dc.contributor.authorChen, N.-
dc.contributor.authorSun, M.-
dc.contributor.authorSantosh, M.-
dc.contributor.authorBa, J.-
dc.date.issued2014-
dc.identifier.citationJournal of Asian Earth Sciences, 2014; 95:33-50-
dc.identifier.issn1367-9120-
dc.identifier.issn1878-5786-
dc.identifier.urihttp://hdl.handle.net/2440/104515-
dc.description.abstractAbstract not available-
dc.description.statementofresponsibilityLu Zhang, Qinyan Wang, Nengsong Chen, Min Sun, M. Santosh, Jin Ba-
dc.language.isoen-
dc.publisherElsevier-
dc.rights© 2014 Elsevier Ltd. All rights reserved.-
dc.source.urihttp://dx.doi.org/10.1016/j.jseaes.2014.05.014-
dc.subjectGeochemistry; Zircon geochronology; Tectonic evolution; Tarim and North China Cratons; Early-Paleoproterozoic-
dc.titleGeochemistry and detrital zircon U-Pb and Hf isotopes of the paragneiss suite from the Quanji massif, SE Tarim Craton: implications for Paleoproterozoic tectonics in NW China-
dc.typeJournal article-
dc.identifier.doi10.1016/j.jseaes.2014.05.014-
pubs.publication-statusPublished-
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]-
Appears in Collections:Aurora harvest 8
Geology & Geophysics publications

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