The formation of a magmatic Cu Ni sulfide deposit in mafic intrusions at the Kalatongke, NW China: Insights from amphibole mineralogy and composition
Abstract
The early Permian Kalatongke CuNi sulfide deposit in the Central Asian Orogenic Belt (CAOB) is the most important CuNi deposit in northern Xinjiang, NW China. It is hosted mainly by mafic intrusions, which is in contrast to deposits in the Eastern Tianshan area of eastern Xinjiang that are hosted mainly by ultramafic intrusions. The controls on sulfide mineralization in the Kalatongke mafic intrusions are poorly constrained relative to the...
Paper Details
Title
The formation of a magmatic Cu Ni sulfide deposit in mafic intrusions at the Kalatongke, NW China: Insights from amphibole mineralogy and composition
Published Date
Jan 1, 2020
Journal
Volume
352-353
Pages
105317 - 105317
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