论文部分内容阅读
本文从邓家山铅锌矿床的地质特征和地球化学特征入手,探讨和论述了该矿床的成因问题,进而提出了沉积—卤水热液再造是该矿床的基本成矿作用。
Based on the geological and geochemical characteristics of the Dengjiashan Pb-Zn deposit, the paper discussed and discussed the genesis of the deposit, and then proposed that the sedimentary-hydrothermal hydrothermal rebuild is the basic metallogeny of this deposit.