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《Geological Review》 1991-01
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THE CHARACTERISTICS AND GEOLOGICAL SIGNIFICANCE MAGMATIC INCLUSIONS IN THE JINCHUAN COPPER-NICKELBEARING ULTRABASIC INTRUSION, GANSU PROVINCE

Yang Xuanzhu, Peng Ligui, Dong Xianyang, Hou Shijun and Gong Zhichao (Xi'an Institute of Geology and Mineral Resources, Chinese Academy of Geological Sciences) An Sanyuan (Xi'an College of Geology)  
Magmatic inclusions were first found in the Jinchuan copper-nickel-bearing ultrabasic intrusion by the authors. The characteristics of magmatic inclusions are systematically studied. The chemical compositions of such crystal-phase daughter minerals olivine, orthopyroxene, clinopyroxene and accessory chrome-spinel and gas-phase volatile components such as F_2, C_(12), CH_4, H_2S, H_2O, SO_2, and CO_2 were measured. The homogenization temperature of magmatic inclusions is in the range of 950—1100℃. The discovery of primary magmatic inclusions in rock-forming minerals suggests a magmatic genesis for the Jinchuan intrusion. Immiscibity in magmatic inclu sions shows that various types of rock and ore were formed by crystallization of melts of different compositions resulting from in-situ liquid unmixing of ferruginous ultrabasic ore-bearing molten magmaas under different physical-chemical conditions. Thes studies are of major significance to the recognition of physicalchemical conditions of rock and ore formation and geneses of rock and ore.
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