Dynamic Magma Conduit System Related to the Jinchuan Ni-Cu Sulfide Deposit, NW China
来源期刊:矿物学报2009年增刊第1期
论文作者:TIAN Yu-long CHEN Lie-meng XIAO Jia-fei SONG Xie-yan
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.
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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.
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