摘要
黑水下口锰矿位于扬子地台西缘之松潘-甘孜地槽马尔康拗陷盆地,锰矿位于三叠系扎尕山组(T z g)中,受地层、构造、岩浆控制明显,属火山沉积受变质型锰矿床。
Heishui manganese deposit is located in the western margin of the Songpan-Ganzi basin.It is influenced by the stratum,geological structure and magma,and it belongs to metamorphic volcanic-sedimentary manganese deposit.
出处
《中国西部科技》
2012年第5期1-2,6,共3页
Science and Technology of West China
基金
国家矿产资源补偿费勘探项目"四川省黑水县下口优质锰矿普查地质报告"(国资发[2003]20号文)资助成果
关键词
锰矿
地质特征
成矿规律
Manganese deposit
Geological characteristics
Mineralization regularity
