Mid-Mesoproterozoic bimodal magmatic rocks in the northern North China craton: implications for magmatism related to breakup of the Columbia supercontinent

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dc.contributor.authorZhang, S.
dc.contributor.authorZhao, Y.
dc.contributor.authorSantosh, M.
dc.date.issued2012
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityShuan-Hong Zhang, Yue Zhao, M. Santosh
dc.identifier.citationPrecambrian Research, 2012; 222-223:339-367
dc.identifier.doi10.1016/j.precamres.2011.06.003
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/104357
dc.language.isoen
dc.publisherElsevier
dc.rights© 2011 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.precamres.2011.06.003
dc.subjectMid-Mesoproterozoic (Ectasian); Bimodal magmatism; Diabase sill (dyke) swarms; Continental rifting; North China Craton; Columbia (Nuna) supercontinent
dc.titleMid-Mesoproterozoic bimodal magmatic rocks in the northern North China craton: implications for magmatism related to breakup of the Columbia supercontinent
dc.typeJournal article
pubs.publication-statusPublished

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