肯皮尔赛铬铁矿南矿区位于肯皮尔赛超基性岩体的东南部。根据物探资料和钻探成果,肯皮尔赛岩体整合产在前寒武纪和奥陶纪岩层之间,是一建造间岩体。岩体的形态与同名复背斜的形态一致。岩体的北段位于肯皮尔赛复背斜的西翼,南段位于复背斜构造的围斜部分。南肯皮尔赛矿区主要由基本上是发育于橄榄岩内、有时发育于缋橄岩内的蛇蚊岩组成。还广 Kempinsai Chromite South Mine is located in the southeast of Kepresi ultramafic rocks. Based on the geophysical data and drilling results, the Kepieixi rock mass is integrated between the Precambrian and Ordovician rock formations and is an inter-building rock mass. The shape of rock mass is consistent with that of the same name complex anticline. The northern part of the rock mass is located in the west wing of the Kepier race anticlinal anticline, and the southern part is located in the anticline part of the complex anticlinal structure. South Kempel Sai mining area is mainly composed of snake mosquito rock is basically developed in the peridotite, sometimes developed in the pluton. Also wide