Xiangshanxi composite Cu-Ni-Ti-Fe deposit belongs to comagmatic evolution product: Evidences from ore microscopy, zircon U-Pb chronology and petrological geochemistry, Hami, Xinjiang, NW China;新疆哈密香山西铜镍-钛铁矿床系同源岩浆分异演化产物——矿相学、锆石U-Pb年代学及岩石地球化学证据

Yanshi Xuebao/Acta Petrologica Sinica

Volumn 26, Issue 2, 2010, Pages 503-522

  Xiao, QingHua ^a,b   Qin, KeZhang ^a   Tang, DongMei ^a   Su, BenXun ^a   Sun, He ^a,b   San, JinZhu ^a,c   Cao, MingJian ^a,b   HUi, WeiDong ^c  

^a BEIJING INSTITUTE OF GEOLOGY FOR MINERAL RESOURCES   (China)

^b UNIVERSITY OF CHINESE ACADEMY OF SCIENCES   (China)

^c Xinjiang Geological Exploration Bureau for Non Ferrous Metals   (China)

Author keywords

Cu Ni sulfide and Ti Fe oxide paragenesis; Geochemistry; Mafic ultramafic complex; Ore microscopy; Xiangshanxi; Xinjiang; Zircon U Pl) chronology

Indexed keywords

EID: 85168643145     PISSN: 10000569     EISSN: 20958927     Source Type: Journal    
DOI: 10.0000/18cc6d11314d47f590352897cec95cc0     Document Type: Article

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