摘要
本文通过烂泥沟金矿区主要控矿断裂F_3的几何形态、内部结构、构造的阐述,及其剪、张、压多次受力、变形与运动特征分析,并从矿与断裂构造的时空等方面论证了构造作用与成矿作用的关系,探讨了构造成矿的机理,提出了构造成矿作用假说。
The mechanism of tectonic mineralization has been studied and the hypothesis of tectonic mineralization has been advanced through the researches of geometric pattern, internal textures and structures,shear,tensile and compressive deformations and tectonic movement many times of main fault F3 controlling gold deposit in Lannigou gold ore -field as well as the relationships of time and space between tectonic movement and gold mineralization.
出处
《贵州地质》
1993年第1期26-34,共9页
Guizhou Geology
