ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.

Parat Abdukadir; Huang Jianhua

Parat Abdukadir, Huang Jianhua. ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.[J]. Geology and Resources, 1997, 6(1): 22-26.

Citation:

Parat Abdukadir, Huang Jianhua. ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.[J]. Geology and Resources, 1997, 6(1): 22-26.

Citation:

Parat Abdukadir, Huang Jianhua. ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.[J]. Geology and Resources, 1997, 6(1): 22-26.

ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.

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Kalatongke sulphide copper and nickle deposit can be divided into three genetic types in intrusive sequence-liquation,injection and hydrothermal superposition types.The last two have a close relation to precious metal mineralization,especially the hydrothermal mineralization.For example, the precious metal(Au,Ag,Pt and Pd)is mainly enriched in high copper massive ore body that separated from the hydrothermal mineralized fluid.The deep melt time of ore-bearing magma in magma house is opposite to the intrusive sequence of each genetic type of ore body. Cu,Ni and precious metal ore body is formed through deep-liquation and mutiple pulsative mineralization.

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ON THE METALLOGEN IC GEOCHEMISTRY OF PRECIOUS METAL OF KALATONGKE Cu-Ni DEPOSIT, XIN JIANG U. Z.

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