摘要
镇康地块位于怒江断裂、龙陵-瑞丽断裂与柯街断裂、南汀河断裂之间。成矿地质条件优越,矿床属与岩浆热液有关的多期、多阶段、多矿质热液型多金属矿床。
The Baoshan - Zhenkang massif is between the Nujiang fault, Longling-Ruili fault and Kejie fault, Nantinghe fault. The geological conditions of metallogenesis is very good. The ore deposit belongs to the multistage, multiple metallogenetic hydrothermal muhimetallic deposit related to the magmatic thermal fluid.
出处
《云南地质》
2007年第1期56-61,共6页
Yunnan Geology
关键词
成矿条件
成矿模式
找矿模型
保山-镇康地场面
滇西南
Metallogenetic Conditions
Metallogenetic Model
Ore-Prospecting Model
Baos- han-Zhenkang Massif
Southwest Yunnan
