摘要
The Jinchuan Ni-Cu sulfide deposits,NW China,are hosted in small ultramafic intrusions that were emplaced into Paleoproterozoic metamorphic rocks. The ultramafic intrusions were previously thought to be the segments of a single elongate intrusion that was dismembered by late faults into eastern and western portions,each of which have distinct stratigraphic sequences.
作者
SONG Xie-yan1,CHEN Lie-meng1,TIAN Yu-long2,XIAO Jia-fei1(1. State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang,550002,China
2. Jinchuan Group Lid,Jinchang,Gansu,737100,China)
出处
《矿物学报》
CAS
CSCD
北大核心
2009年第S1期82-82,共1页
Acta Mineralogica Sinica
