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《成都地质学院学报》 1987-03
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PHYSICOCHEMICAL CONDITION OF ROCK FORMATION AND MINERALIZATION OF HUANGSHANDONG MAGMATOGENIC SULFIDE DEPOSIT HAMI, XINJIANG, CHINA

Wang Runmin (Chengdu College of Geology)Li Chusi (Beijing Graduate School of Wuhan College of Geology)  
Huangshandong deposit occurred within the North Tianshan geo synclinal fold belt and is a typical representative of magmatogenic Cu-Ni sulfide occurrences in the Tudun-Huangshan metallogenic province.On the basis of mineralochemistry study, it is suggested that the magma crystallized under the condition of t=1647—900℃, f_(H2O)=4—5 kbar, fo_2=10~(-10.89), and the temperature of crystallization of sulfides was more than 450℃.
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