摘要
武当隆起为银金多金属矿床(点)的重要成矿区,形成武当隆起西缘成矿带,构造对该矿带矿床的形成和产出起着重要作用。早期伸展构造形成的滑脱构造面基本控制了该区金银、多金属矿床(点)的产出和分布,后期逆冲推覆构造对前期形成的矿体或矿化体进行叠加、改造,并再次富集定位。
The Wudang upheaval is an important metallogenic area of the Ag-Au-Polymetallic ore deposits. The ore deposits mainly distribute in the west edge of Wudang upheaval and form the western metallogenie belt. The structure plays a major role for occurrence of ore deposits, and detachment structural surfaces of early extension structure control the distribution of the ore deposits. The ore bodies which had formed were superimposed and reformed by the later nappe structure, and then had been enriched.
出处
《黄金科学技术》
2008年第4期4-8,共5页
Gold Science and Technology
基金
国土资源部"国土资源大调查项目"(编号:DK9902035)资助
关键词
武当隆起
银金多金属矿床
滑脱构造面
逆冲推覆构造
控矿作用
Wudang upheaval
Ag-Au-Polymetallic ore deposits
Detachment structural surfaces
Nappe structure
Structure control
