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GEOLOGIC CHARACTERS OF QIAOLAKE GOLD DEPOSIT OF XINJIANG AND ITS GENETIC ANALYSIS

Zeng Xiao

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Abstract

Qiaolake gold deposit occurs in Yishijilike later paleozoic tectonic magma rock belt.On the view of the characteristics of hypabyssal super hypabyssal intrusive,alteration zoning and element geochemistry,it is considered that the genesis of the deposit is closely associated with strong strain structure zones and hypabyssal super hypabyssal intrusive.It belongs to hypabyssal lower to mesothermal type gold deposit.An exploration model for the deposit has been built according to metallogenic characters.

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What this paper is about

Qiaolake gold deposit occurs in Yishijilike later paleozoic tectonic magma rock belt.On the view of the characteristics of hypabyssal super hypabyssal intrusive,alteration zoning and element geochemistry,it is considered that the genesis of the deposit is closely associated with strong strain structure zones and hypabyssal super hypabyssal intrusive.It belongs to hypabyssal lower to mesothermal type gold deposit.An exploration model for the deposit has been built according to metallogenic characters.

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Available abstract

Qiaolake gold deposit occurs in Yishijilike later paleozoic tectonic magma rock belt.On the view of the characteristics of hypabyssal super hypabyssal intrusive,alteration zoning and element geochemistry,it is considered that the genesis of the deposit is closely associated with strong strain structure zones and hypabyssal super hypabyssal intrusive.It belongs to hypabyssal lower to mesothermal type gold deposit.An exploration model for the deposit has been built according to metallogenic characters.

Key concepts: Geology, Mesothermal, Paleozoic, Geochemistry, Magma, Tectonics, Petrology, Quartz

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