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托库孜巴伊金矿赋矿岩层为中泥盆统阿勒泰组上亚组第二岩性段第二岩性层的绢云绿泥千枚岩和褐铁矿化变长石石英砂岩,矿体受F9、F10两条脆韧性断层控制。笔者通过对托库孜巴伊金矿的构造特征、控矿因素及矿床成因的系统研究,总结了找矿标志,进而指出了找矿方向。
The Tukuzi-Bai gold ore deposit is a sericite-chitite phyllite and limonite-altered variegated quartzite sandstone of the second lithologic layer of the Upper Cretaceous Altay Formation in the Middle Devonian. Body by F9, F10 two brittle and ductile fault control. Based on the systematic study on the tectonic characteristics, ore-controlling factors and genesis of the Tokuj-Iraqi gold deposit, the author summarizes the prospecting signs and then points out the prospecting direction.