摘要
铁腊曲铅银矿位于德钦—维西有色金属成矿带内,是三江成矿带中铅、锌、银矿的富集区域之一。初步认为矿床成因受构造破碎带控制,与地下热卤水溶滤作用有关的热液型铅银多金属矿床。
The Tielaqu Pb-Ag Orefield of Jianchuan is in the Deqin-Weixi nonferrous metallogenetic zone,which is one of the Pb-Zn-Ag concentration area in the three-river metallogenetic zone.Because of the special tectonic position of it,the geological structure is complicated,magmatism is intense and frequent and geological condition of metallogenesis is good.We think preliminarily that the ore deposit is a hydrothermal Pb-Ag multimetallic deposit controlled by structural fracture zone and related to the solution and leaching of underground thermal brine in genesis.
出处
《云南地质》
2011年第2期141-143,共3页
Yunnan Geology
关键词
铅银多金属矿
热卤水溶滤作用
构造破碎带控矿
层位、岩性赋矿
云南剑川铁腊曲
Pb-Ag Multimetallic Deposit
Solution ＆ Leaching of Thermal Brine
Ore Control of Structural Fracture Zone
Ore-Bearing of Horizon and Lithological Character
Tielaqu
Jianchuan
Yunnan
