摘要
盐巴箐铜矿赋存于下元古界大红山群曼岗河组下部,河口背斜轴部,呈似层状、透镜状与围岩基本上整合产出。为海相火山沉积变质铜矿床。
Salt Jing copper deposit occurs in Lower Proterozoic Dahongshan group Manchester Gang River group lower estuary anticline,stratoid and lenticular and surrounding rock basically integrated output.For marine volcanic sedimentary metamorphic copper deposits.
出处
《世界有色金属》
2017年第9期43-44,共2页
World Nonferrous Metals
关键词
纳长片岩
沉积变质矿床
铜矿
云南新平
Nachang schist
sedimentary metamorphic deposit
copper deposit
Yunnan Province
