1.23 Ga mafic dykes in the North China Craton and their implications for the reconstruction of the Columbia supercontinent

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dc.contributor.authorWang, W.
dc.contributor.authorLiu, S.
dc.contributor.authorSantosh, M.
dc.contributor.authorZhang, L.
dc.contributor.authorBai, X.
dc.contributor.authorZhao, Y.
dc.contributor.authorZhang, S.
dc.contributor.authorGuo, R.
dc.date.issued2015
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityWei Wang, Shuwen Liu, M. Santosh, Lifei Zhang, Xiang Bai, Yue Zhao, Shuanhong Zhang, Rongrong Guo
dc.identifier.citationGondwana Research, 2015; 27(4):1407-1418
dc.identifier.doi10.1016/j.gr.2014.02.002
dc.identifier.issn1342-937X
dc.identifier.issn1878-0571
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/103043
dc.language.isoen
dc.publisherElsevier
dc.rights© 2014 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.gr.2014.02.002
dc.subjectMafic dykes; Geochronology; Mantle plume; Columbia–Rodinia transition; North China Craton
dc.title1.23 Ga mafic dykes in the North China Craton and their implications for the reconstruction of the Columbia supercontinent
dc.typeJournal article
pubs.publication-statusPublished

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