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

Tang, D.Qin, K.Su, B.Sakyi, P.Liu, Y.Mao, Q.Santosh, M.Ma, Y.2018-05-072018-05-072013Lithos, 2013; 170-171:144-1630024-49371872-6143http://hdl.handle.net/2440/111920Abstract not availableen© 2013 Elsevier B.V. All rights reserved.Xiangshanzhong; mafic–ultramafic intrusion; clinopyroxene; parental magma; emplacement mechanism; Central Asian Orogenic BeltMagma source and tectonics of the Xiangshanzhong mafic-ultramafic intrusion in the Central Asian Orogenic Belt, NW China, traced from geochemical and isotopic signaturesJournal article003004424610.1016/j.lithos.2013.02.0130003197901000092-s2.0-84876322918235027Santosh, M. [0000-0002-1073-8477]