First report of Paleoproterozoic incipient charnockite from the North China Craton: implications for ultrahigh-temperature metasomatism

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dc.contributor.authorYang, Q.
dc.contributor.authorSantosh, M.
dc.contributor.authorTsunogae, T.
dc.date.issued2014
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityQiong-Yan Yang, M. Santosh, Toshiaki Tsunogae
dc.identifier.citationPrecambrian Research, 2014; 243:168-180
dc.identifier.doi10.1016/j.precamres.2014.01.004
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/104554
dc.language.isoen
dc.publisherElsevier
dc.rights© 2014 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.precamres.2014.01.004
dc.subjectIncipient charnockite; petrology; zircon U–Pb geochronology; Paleoproterozoic; North China Craton
dc.titleFirst report of Paleoproterozoic incipient charnockite from the North China Craton: implications for ultrahigh-temperature metasomatism
dc.typeJournal article
pubs.publication-statusPublished

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