Ore-Control Factors and Genetic Type for the Zhawala Gold Deposit in Batang, Sichuan
详细信息   
摘要


     The Zhawala gold deposit is confined to the Permian-Lower Triassic marble and controlled by nearly north-southern shear fractured alteration zones. The deposit was formed by Indo-Chinese magmatism and faulting and was not in direct relation with skarnization. The deposit belongs to medium-lower temperature tectonic-hydrothermal alteration type with prospect of medium-large deposit in the north-southern fractured alteration zone around the magmatic mass.

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