Crust-mantle interaction beneath the Luxi Block, eastern North China Craton: evidence from coexisting mantle- and crust-derived enclaves in a quartz monzonite pluton

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dc.contributor.authorLan, T.
dc.contributor.authorFan, H.
dc.contributor.authorSantosh, M.
dc.contributor.authorHu, F.
dc.contributor.authorYang, K.
dc.contributor.authorYang, Y.
dc.contributor.authorLiu, Y.
dc.date.issued2013
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityTing-Guang Lan, Hong-Rui Fan, M. Santosh, Fang-Fang Hu, Kui-Feng Yang, Yue-Heng Yang, Yongsheng Liu
dc.identifier.citationLithos, 2013; 177:1-16
dc.identifier.doi10.1016/j.lithos.2013.05.017
dc.identifier.issn0024-4937
dc.identifier.issn1872-6143
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/112201
dc.language.isoen
dc.publisherElsevier
dc.rights© 2013 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.lithos.2013.05.017
dc.subjectQuartz monzonite; enclave; crustal reactivation; crust–mantle interaction; North China Craton
dc.titleCrust-mantle interaction beneath the Luxi Block, eastern North China Craton: evidence from coexisting mantle- and crust-derived enclaves in a quartz monzonite pluton
dc.typeJournal article
pubs.publication-statusPublished

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