摘要
巴阿泽锰矿位于瓦钵梁子—四美沟复背斜东部倾没端。通过对黑水县巴阿泽锰矿床的综合研究,该矿床的含矿层位为菠茨沟组中段(PTb2)。矿区共圈定2条矿体。同时对该区的矿床地质特征及成矿规律进行了分析,认为该矿床属于沉积-受变质型矿床,并归纳总结出三条找矿标志。
Bar Azeri Mn deposit occurs in the plunging end of the Waboliangzi-Simeigou composite anticline. The deposit consists of 2 orebodies which are confined to the Lower Triassic Bocigou Formation. This paper deals with its geological features and believes it is a sedimentary-metamorphosed deposit.
出处
《四川地质学报》
2015年第1期30-33,共4页
Acta Geologica Sichuan
