Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/109842
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dc.contributor.authorMa, X.en
dc.contributor.authorShu, L.en
dc.contributor.authorSantosh, M.en
dc.contributor.authorLi, J.en
dc.date.issued2012en
dc.identifier.citationPrecambrian Research, 2012; 206-207:1-16en
dc.identifier.issn0301-9268en
dc.identifier.issn1872-7433en
dc.identifier.urihttp://hdl.handle.net/2440/109842-
dc.description.abstractAbstract not availableen
dc.description.statementofresponsibilityXuxuan Ma, Liangshu Shu, M. Santosh, Jinyi Lien
dc.language.isoenen
dc.publisherElsevieren
dc.rights© 2012 Elsevier B.V. All rights reserved.en
dc.subjectU–Pb geochronology; crustal evolution; Baluntai; Central Tianshan; Tarim Block; supercontinenten
dc.titleDetrital zircon U-Pb geochronology and Hf isotope data from Central Tianshan suggesting a link with the Tarim Block: implications on Proterozoic supercontinent historyen
dc.typeJournal articleen
dc.identifier.doi10.1016/j.precamres.2012.02.015en
pubs.publication-statusPublisheden
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]en
Appears in Collections:Aurora harvest 3
Geology & Geophysics publications

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