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东准噶尔地区分布有索尔库都克、哈腊苏-卡拉先格尔、乌伦布拉克-溴水泉、塔黑尔巴斯套与琼河坝5条斑岩铜矿带,分为构造叠加改造型斑岩铜矿、断裂构造背景下的斑岩铜矿与和尔赛型斑岩铜矿3种构造类型.构造叠加改造型斑岩铜矿受后期韧性变形构造改造、硫化物沿片理带富集,黄铜矿细脉主要分布于片理带中相对较弱的破劈理中,铜矿体总体产状与片理带产状一致.断裂构造背景下的斑岩铜矿,含矿斑岩体呈岩枝状产出,矿化脉体及伴生蚀变与断裂构造关系密切.和尔赛型斑岩铜矿,具典型斑岩铜矿与岩浆融离型矿床的双重特征,是一个较特殊的斑岩铜矿.
There are five porphyry copper belt belts in the East Junggar area, including Sorkurduk, Harasso-Kaila-Sengel, Ulun Burak-Bromo-Hydrullus, Tahel Bassett and Qiongheba, which are divided into tectonic superposition The altered porphyry copper deposit, the porphyry copper deposit under the fault tectonic setting and the Heersai porphyry copper deposit.The structural alteration porphyry copper deposit is rebuilt by the later ductile deformation tectonics, With the enrichment of chalcopyrite vein, the chalcopyrite vein is mainly distributed in the relatively weaker broken cleavage in the belt, and the general occurrence of copper ore body is consistent with that of the carded belt. The porphyry copper deposits in the fault structure background The ore-bearing porphyry bodies are in the form of rock-like dendrites, and the mineralized veins and associated alteration are closely related to the fault structure. The dual characteristics of the Heersai porphyry copper deposit, with typical porphyry copper deposits and magmatic melt deposits, are A more special porphyry copper mine.