摘要
安妥岭钼矿位于燕辽钼(铜)成矿带南端,与附近的野弧斑岩型钼矿等具有相同的地质背景和成矿条件。文章阐述了古结晶基底、中生代岩体以及NNE、NW和近EW向构造与成矿的关系,提出安妥岭钼矿是在斑岩型矿床基础上,叠加了主要沿NW向构造发育的岩浆热液成矿作用所形成的具有复杂成矿系列的非典型斑岩钼矿床。
Antuoling molybdenum deposit locates in south part ol Yanllao Molybdenum（Cu） minerailzauon belt. It has the same geological background and mineralization condition with the nearby Yehu porphyrite molybdenum deposit. Relationship among mineralization, ancient crystal basement, the Mesozoic rockbody and the structures with the trend of NNE, NW and nearly EW are illustrated in this paper. It points out that Antuoling molybdenum deposit is untypical porphyry--type deposit with complex mineralization series, which is stacked by the magma hydrothermal mineralization occuring along the NW trend structure.
出处
《山东国土资源》
2009年第9期20-25,共6页
Shandong Land and Resources
关键词
钼矿
燕辽钼(铜)成矿带
斑岩型矿床
成矿系列
叠加成矿作用
冀西安妥岭
Molybdenum deposit
Yanliao Mo（Cu） mineralization belt
porphyry- type deposit
minerali-zation series
stacking mineralization
Antuoling in estern Hebei province
