摘要
玲珑断裂和破头青断裂是区内一级矿田构造,属引裂构造.它的生成经历了多期次的构造演化.由于受力性质的不同,形成了一系列规模不同、方向各异的容矿裂隙.引裂构造与容矿裂隙交汇处常形成矿体、矿柱.
The Linglong and the Potouqing fractures, both being first order ore field structures in this district,belong to induced fracture structure. Their formation had experienced a multistage structural evolution.Because of the forces they experienced being different in nature, a series of ore-hosting fractures of different scales and directions were formed. At the intersection of the induced fracture structure and ore hosting fracture, ore bodies or ore pillars may be found.
出处
《地质与勘探》
CAS
CSCD
北大核心
1989年第12期17-21,共5页
Geology and Exploration
