摘要
滇东南薄竹山地区是矽卡岩型白钨矿矿床的重要汇集区之一。研究薄竹山地区典型矿区矿床地质特征,总结出矽卡岩型白钨矿矿床受花岗岩与碳酸盐岩地层接触带构造控制,花岗岩为成矿提供了丰富的成矿物质来源,碳酸盐岩地层为成矿提供了钙源。
Bozhushan mining area in southeastern Yunnan is an important part of skarn-type seheelite deposit. By researching the geological characteristics of the typical deposits, summarizes this ore deposits are obviously tec- tonic controlled by the contact zone of granites and Carbonate Formations. Granites provided some ore-forming ma- terieds source and carbonates provided some source of calcium.
出处
《科学技术与工程》
北大核心
2014年第9期131-135,共5页
Science Technology and Engineering