Metallogeny during continental outgrowth in the Columbia supercontinent: isotopic characterization of the Zhaiwa Mo-Cu system in the North China Craton

dc.contributor.authorDeng, X.
dc.contributor.authorChen, Y.
dc.contributor.authorSantosh, M.
dc.contributor.authorZhao, G.
dc.contributor.authorYao, J.
dc.date.issued2013
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityX.H. Deng, Y.J. Chen, M. Santosh, G.C. Zhao, J.M. Yao
dc.identifier.citationOre Geology Reviews, 2013; 51:43-56
dc.identifier.doi10.1016/j.oregeorev.2012.11.004
dc.identifier.issn0169-1368
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/112601
dc.language.isoen
dc.publisherElsevier
dc.rights© 2012 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.oregeorev.2012.11.004
dc.subjectZhaiwa Mo–Cu deposit; isotope geochemistry; molybdenite Re–Os age; Xiong'er group; North China Craton; continental arc; continental outgrowth
dc.titleMetallogeny during continental outgrowth in the Columbia supercontinent: isotopic characterization of the Zhaiwa Mo-Cu system in the North China Craton
dc.typeJournal article
pubs.publication-statusPublished

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