【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 Ce
【机 构】
：
State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Scienc
【出 处】
：
International Workshop on: Ophiolites, Mantle Processes and
论文部分内容阅读
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).Questions for genetic link between these deposits and the Early Permian Tarim mantle plume are:(1)Early Permian Ni-Cu sulfide mineralizedmafic-ultramafic complexes have been also found in locations 1500-2000 km to the east along the southern margin of the Central Asian Orogenic Belt and(2)Similar Silurian and Devonian complexes also occur in adjacent West Tianshan and Beishan Belt.
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