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Charnockite magmatism during a transitional phase: Implications for late Paleoproterozoic ridge subduction in the North China Craton

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dc.contributor.authorYang, Q.
dc.contributor.authorSantosh, M.
dc.date.issued2015
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityQiong-Yan Yang, M. Santosh
dc.identifier.citationPrecambrian Research, 2015; 261:188-216
dc.identifier.doi10.1016/j.precamres.2015.01.014
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/100695
dc.language.isoen
dc.publisherElsevier
dc.rights© 2015 Elsevier B.V. All rights reserved
dc.source.urihttps://doi.org/10.1016/j.precamres.2015.01.014
dc.subjectPetrology; geochemistry; zircon U–Pb geochronology and Lu–Hf isotopes; Charnockite; North China Craton
dc.titleCharnockite magmatism during a transitional phase: Implications for late Paleoproterozoic ridge subduction in the North China Craton
dc.typeJournal article
pubs.publication-statusPublished

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