甘肃省文县清水坪重晶石矿矿体特征及成矿原因分析

Analysis of Gansu Province, Wenxian water Ping barite ore characteristics and metallogenic reasons

矿区地处秦岭东西向构造带南部,区域构造属西藏—三江造山系巴颜喀拉地块东端,地层区划属于扬子地层区、西秦岭分区、文县-康县小区。本文对清水坪重晶石矿矿体特征及成矿原因进行来研究分析。

The mining area is located in the south of the Qinling East-west tectonic belt. The regional structure belongs to the eastern end of the Bayan Hara block of Tibet-Sanjiang orogenic system, and the stratigraphic division belongs to Yangtze strata, West Qinling and Wenxian-Kangxian districts. In this paper, the ore body characteristics and metallogenic factors of the Qingshuping barite deposit are studied and analyzed.