Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/112469
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dc.contributor.authorZhao, P.en
dc.contributor.authorYuan, S.en
dc.contributor.authorMao, J.en
dc.contributor.authorSantosh, M.en
dc.contributor.authorZhang, D.en
dc.date.issued2017en
dc.identifier.citationLithos, 2017; 292-293:132-145en
dc.identifier.issn0024-4937en
dc.identifier.issn1872-6143en
dc.identifier.urihttp://hdl.handle.net/2440/112469-
dc.description.abstractAbstract not availableen
dc.description.statementofresponsibilityPanlao Zhao, Shunda Yuan, Jingwen Mao, M.Santosh, Dongliang Zhangen
dc.language.isoenen
dc.publisherElsevieren
dc.rights© 2017 Elsevier B.V. All rights reserveden
dc.subjectQin–Hang metallogenic belt; magmatic source; zircon geochronology and Hf–Oisotopes; petrogenesis; porphyry-skarn Cu depositsen
dc.titleZircon U–Pb and Hf–O isotopes trace the architecture of polymetallic deposits: a case study of the Jurassic ore-forming porphyries in the Qin–Hang metallogenic belt, Chinaen
dc.typeJournal articleen
dc.identifier.rmid0030078539en
dc.identifier.doi10.1016/j.lithos.2017.08.016en
dc.identifier.pubid389173-
pubs.library.collectionGeology & Geophysics publicationsen
pubs.library.teamDS10en
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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