摘要
程巴铜钼多金属矿床位于冈底斯成矿带东段南缘。矿体呈似层状、透镜状产出于似斑状二长花岗岩及石英钠长斑岩外接触带的矽卡岩、大理岩之中,为典型斑岩-矽卡岩型矿床。近几年勘查工作表明矿区深部具有较大的找矿空间。
Chengba Cu-Mo multimetallic deposit is in the S margin of E Gangdise metallogenetic zone. The ore body is stratoid, lenticular, in the skarn, marble of outer contact of quasi-porphyritic adamellite and quartz albite porphyry. It is a typical porphyry-skarn type ore deposit. The exploration in recent years shows there is the wide prospecting space in the deep.
出处
《云南地质》
2016年第1期69-72,共4页
Yunnan Geology
