摘要
本文阐明四川某铅锌矿矿床的构造特征,并展示了该矿床主要断裂益门断裂(F1)、EW向的隐伏断裂(F2)和F3等深大断裂以及它们之间的相互关系。其中F1贯穿至基底,起导矿作用;F2起容矿和导矿作用。同时F2的破碎带为矿液提供了非常有利的成矿空间,成矿物质附近聚集成矿。综上,可见:在成矿过程中,构造起了至关重要的作用。
In this paper,I describe the structural feature of Tianbaoshan Deposit in Hui Li Sichuan,and show the relations among yimen falut（F1）,buried falut（F2） and F3.F1 which reaches the crust leaded the ore solution up and down.F2 leaded and compounded ore solution.Fracture zone provided advantageous spaces to ore solution to deposit.Generally,we could make the conclusion：in the formation of Tianbaoshan Pb-Zn deposit,the structure played a important role.
出处
《内蒙古石油化工》
CAS
2010年第18期74-76,共3页
Inner Mongolia Petrochemical Industry
关键词
构造特征
构造控矿
铅锌矿
会理天宝山
Structural feature
Mineraling-controlling
Pb-Zn deposit
Tianbaoshan in Hui Li
