Generation of Permian Ni-Cu Sulfide Deposits in the East Tianshan(NW China) by Syn-collisional Mantle Derived Magmatism  

作　　者：SONG Xieyan CHEN Liemeng DENG Yufeng XIE Wei 

机构地区：[1]State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences

出　　处：《Acta Geologica Sinica(English Edition)》2015年第A02期87-88,共2页地质学报（英文版）

摘　　要：A series of Ni-Cu sulfide deposits hosted in Early Permian mafic-ultramafic complexes occur along the -500 km long linear Huangshan-Jingerquan belt in the East Tianshan at the southern margin of the Central Asian Orogenic Belt （Fig. 1） （Zhou et al., 2004; Song and Li,2009; Song et al., 2011 ; Qin et al., 2011 ; Deng et al., 2014）.A series of Ni-Cu sulfide deposits hosted in Early Permian mafic-ultramafic complexes occur along the -500 km long linear Huangshan-Jingerquan belt in the East Tianshan at the southern margin of the Central Asian Orogenic Belt （Fig. 1） （Zhou et al., 2004; Song and Li,2009; Song et al., 2011 ; Qin et al., 2011 ; Deng et al., 2014）.

分 类 号：P618.41[天文地球—矿床学] P588.124[天文地球—地质学]