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The Baishiquan mafic–ultramafic intrusions associated with magmatic Ni–Cu–(PGE) sulfide deposit are located in the northern margin of the Central Tianshan Block in northern Xinjiang, NW China. The intrusions consist of olivine pyroxenite, pyroxene peridotite, troctolite, hornblendite, gabbro and diorite. The peridotite and pyroxenite are the main host rock for the Cu–Ni ores. The crystallization sequence...
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