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落凼矿区作为含铜矿重要产出地,对其进行地质构造研究以及矿床成因分析有着极为重要的意义,对于今后的采矿作业有着非常大的指导意义。随着我国对金属铜的开采不断增加,研究矿区地质构造所具有的特征以及矿床成因对今后的开采有着极大的作用。本文就实际开采地进行细致的研究,对落凼矿区所具有的地质构造形式以及特征加以分析,同时对矿床成因加以分析,从而对矿床的成矿模式加以一定的假设。
As an important copper-bearing ore-producing area, the Cotai mining area is of great significance to geological research and genesis analysis of the deposit, and has very great guiding significance for future mining operations. With the increasing exploitation of metallic copper in our country, it is very important to study the characteristics of the geological structure of the mining area and the genesis of the deposit for the future exploitation. In this paper, the detailed study on the actual mining area is carried out. The geological structure forms and characteristics of the Orangiang mining area are analyzed. At the same time, the genesis of the deposit is analyzed to make certain assumptions on the metallogenic model of the deposit.