摘要
克因布拉克铜锌矿区位于克兰复向斜中的冲呼尔向斜的南东部,黑流滩大断裂的西南侧。矿区产于拉张期的下泥盆统的康布铁堡组陆源碎屑-火山岩建造中。本文以铜锌为主攻矿种在该区域开展土壤地球化学测量及对已发现的矿化异常进行评价,圈定重点工作区,为下一步找矿工作提供依据,并探讨土壤地球化学测量手段在该区找矿中的应用。
The Keinbulake Copper-Zinc Mine Area is located in the southwest side of the Oliver River, which is located in the oblique slanting of the Cromf in the south and east. The mine is located in the construction of the debris-volcanic rocks D1 k. In this paper, the soil and geochemical measurements of the soil and the mineralization anomalies were evaluated in this area, and the key target areas were identified, which provided the basis for the next prospecting work and to discusses the soil geochemical survey methods in the application of the prospecting in the area.
出处
《四川有色金属》
2017年第3期5-8,共4页
Sichuan Nonferrous Metals
