Magma source and tectonics of the Xiangshanzhong mafic-ultramafic intrusion in the Central Asian Orogenic Belt, NW China, traced from geochemical and isotopic signatures

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dc.contributor.authorTang, D.
dc.contributor.authorQin, K.
dc.contributor.authorSu, B.
dc.contributor.authorSakyi, P.
dc.contributor.authorLiu, Y.
dc.contributor.authorMao, Q.
dc.contributor.authorSantosh, M.
dc.contributor.authorMa, Y.
dc.date.issued2013
dc.description.abstractAbstract not available
dc.description.statementofresponsibilityDongmei Tang, Kezhang Qin, Benxun Su, Patrick Asamoah Sakyi, Yongsheng Liu, Qian Mao, M. Santosh, Yuguang Ma
dc.identifier.citationLithos, 2013; 170-171:144-163
dc.identifier.doi10.1016/j.lithos.2013.02.013
dc.identifier.issn0024-4937
dc.identifier.issn1872-6143
dc.identifier.orcidSantosh, M. [0000-0002-1073-8477]
dc.identifier.urihttp://hdl.handle.net/2440/111920
dc.language.isoen
dc.publisherElsevier
dc.rights© 2013 Elsevier B.V. All rights reserved.
dc.source.urihttps://doi.org/10.1016/j.lithos.2013.02.013
dc.subjectXiangshanzhong; mafic–ultramafic intrusion; clinopyroxene; parental magma; emplacement mechanism; Central Asian Orogenic Belt
dc.titleMagma source and tectonics of the Xiangshanzhong mafic-ultramafic intrusion in the Central Asian Orogenic Belt, NW China, traced from geochemical and isotopic signatures
dc.typeJournal article
pubs.publication-statusPublished

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