摘要
矿床与华力西期超基性—基性—中性岩浆杂岩关系密切,成矿专属性明显。先期矿浆在杂岩体中初步熔离富集,后期矿浆在压力作用下沿断裂贯入,经期后热液改造再富集成矿。
The ore deposit is in a close relation to the Variscan ultrabasic - basic - intermediate magmatic complex, with clear metallogenetic specialization. The earlier ore magma is immiscibly separated and concentrated preliminarily in the complex. The later one injectes in the fault under the pressure, then concentration and metal- logenesis take place after the post- hydrothermal reformation,
出处
《云南地质》
2011年第3期285-288,共4页
Yunnan Geology
关键词
铜镍矿
相变带外侧
片理化断裂带
深部贯入成矿
云南金平阿德博
Cu - Ni Deposit
Outer Side of Facies Change Zone
Schistositized Fault Zone
Metallogenesisof Deep Ore Magma Injection
Adebo, Jinping, Yunnan
