简介概要

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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Dynamic Magma Conduit System Related to the Jinchuan Ni-Cu Sulfide Deposit, NW China

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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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