摘要
北达巴特斑岩铜钼矿产于华力西期流纹斑岩中,矿体呈脉状,铜矿体地表为氧化物,钼矿体主要赋存于深部的流纹斑岩中,其矿化作用呈上铜下钼的双层矿化结构模式,矿化为细脉浸染状。矿床的成因类型为斑岩型铜钼矿。
The Beidabate porphyry Cu-Mo deposit occurs in Variscan rhyolite porphyry with its orebodies presenting in veins. The surface of Cu orebody is covered with oxide, while the Mo orebody mainly locates in the rhyolite porphyry of deep part. The mineralization presents a double-layer mineralizing structure mode with the upside being Cu mineralization and the underside being Mo mineralization, and occurs in veinlet disseminating state. The genesis type of this deposit is porphyry Cu-Mo deposit.
出处
《矿产与地质》
2008年第1期10-14,共5页
Mineral Resources and Geology
关键词
斑岩铜(钼)矿
地质特征
成因
北达巴特
porphyry Cu （Mo） deposit, geological characteristics, genesis, Beidabate
