Characteristics of the Huilushan Gold Deposit in Tuoli County,Xinjiang
The mining area is located in the Dalabute Late Paleozoic backarc basin of the Junggar Basin.The exposed strata in the mining area are the Lower Subgroup of the Lower Carboniferous Tailegula Formation,which consists of a set of volcanic clastic rock formations.The exposed Late Carboniferous shallow to ultra shallow facies diabase rock masses are closely related to mineralization.There are 5 gold ore bodies distributed in the mining area,and the ore structure mainly includes fragmented structure,vein structure,etc.The ore structure mainly includes angular gravel structure,disseminated structure,etc.The natural type of ore is mainly gold bearing pyrite magnetite quartz vein type.The formation of the deposit is due to the high-to medium temperature hydrothermal filling metasomatic gold bearing quartz vein type deposit.
backarc basinTailegula FormationDiabase rock massGenesis of mineral deposits
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