Neoarchean to Paleoproterozoic continental growth in the southeastern margin of the North China Craton: geochemical, zircon U-Pb and Hf isotope evidence from the Huoqiu complex

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dc.contributor.authorLiu, L.
dc.contributor.authorYang, X.
dc.contributor.authorSantosh, M.
dc.contributor.authorAulbach, S.
dc.date.issued2015
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityLei Liu, Xiaoyong Yang, M. Santosh, S. Aulbach
dc.identifier.citationGondwana Research, 2015; 28(3):1002-1018
dc.identifier.doi10.1016/j.gr.2014.08.011
dc.identifier.issn1342-937X
dc.identifier.issn1878-0571
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/116298
dc.language.isoen
dc.publisherElsevier
dc.relation.grant41090372
dc.relation.grant40921002
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.2014.08.011
dc.subjectZircon geochronology; hafnium isotopes; geochemistry; crustal evolution; North China Craton
dc.titleNeoarchean to Paleoproterozoic continental growth in the southeastern margin of the North China Craton: geochemical, zircon U-Pb and Hf isotope evidence from the Huoqiu complex
dc.typeJournal article
pubs.publication-statusPublished

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