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Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/112469
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dc.contributor.authorZhao, P.-
dc.contributor.authorYuan, S.-
dc.contributor.authorMao, J.-
dc.contributor.authorSantosh, M.-
dc.contributor.authorZhang, D.-
dc.date.issued2017-
dc.identifier.citationLithos, 2017; 292-293:132-145-
dc.identifier.issn0024-4937-
dc.identifier.issn1872-6143-
dc.identifier.urihttp://hdl.handle.net/2440/112469-
dc.description.abstractAbstract not available-
dc.description.statementofresponsibilityPanlao Zhao, Shunda Yuan, Jingwen Mao, M.Santosh, Dongliang Zhang-
dc.language.isoen-
dc.publisherElsevier-
dc.rights© 2017 Elsevier B.V. All rights reserved-
dc.source.urihttp://dx.doi.org/10.1016/j.lithos.2017.08.016-
dc.subjectQin–Hang metallogenic belt; magmatic source; zircon geochronology and Hf–Oisotopes; petrogenesis; porphyry-skarn Cu deposits-
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, China-
dc.typeJournal article-
dc.identifier.doi10.1016/j.lithos.2017.08.016-
dc.relation.grantYYWF-201711-
dc.relation.grantK1204-
dc.relation.grant41373047-
dc.relation.grant41672095-
dc.relation.grant41173052-
pubs.publication-statusPublished-
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]-
Appears in Collections:Aurora harvest 3
Geology & Geophysics publications

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