摘要
研究区位于大兴安岭火山岩带中南部,中新生代火山作用强烈,不同的火山作用方式,伴随着不同的成矿作用,而昌图锡力锰铅锌银矿的形成可能与熔浆经分异、熔离或交代置换围岩中有用组分,贯入表层中的裂隙、断层或直接喷出火口有关。
The study area is located in the greater hinggan mountains South-central volcanic rock belt, the Cenozoic volcanism is strong, and different ways of volcanism, with different mineralization, and the formation of Changtuxili Mn- Ag-Pb-ZN silver force may be related to magma differentiation, liquation or replacement of displacement of surrounding rock of useful components, injection surface fissure, fault or directly in the overflowing crater.
出处
《世界有色金属》
2017年第1期255-256,共2页
World Nonferrous Metals