- 责任者：Chen Chao (College of Resources ; Shijiazhuang University of Economics ; Shijiazhuang 050031 ; China) ; Niu Shuyin
- 刊名：Geology and Prospecting
- 出版年：2013
- 卷期：49(5)
- 关键词：铜矿 ; copper ores ; 钼矿 ; molybdenum ores ; 河北 ; Hebei Province
- 页码：p.861-871
- 图表：4 illus., 2 tables, 24 refs.
- 分类号：1001
- issnNo：ISSN0495-5331
- isbnNo：CN11-2043/P
The Mujicun copper （molybdenum） deposit is a large copper （molybdenum） -gold and silver polymetallic ore field in the northern Taihang Mountains, which is located in a secondary faulted basin in the upper wall of the detachment zone on the west of the Laiyuan complex rock body with a dumbbell shape, the northern section of Fuping mantle branch structure. This paper analyzes the rock-controlling function and ore-controlling model of the structures in this area based on the metallogenic geological background and latest exploration results. It is concluded thai the deposit was controlled by dio- rite-porphyrite bodies, which intruded in the faulted basin, and its related fracture tectonic system as well as strong wall rock alteration zones. The Muji- con porphyry copper （molybdenum） deposits, skarn iron-copper deposits （such as Futuyu）, and hydrothermal vein Lead-zinc-silver polymetallic deposits （ such as He＇ ergou） jointly constituted a large polymetallic ore field with typical characteristics of serial mineralization.