摘要
辽西南部，一组ＮＷ 向断裂与一组近ＥＷ 向平行断裂控制了多金属矿床的产出，形成矿床集中区。
In Southwest Liaoning,a group of faults in the trend of NW is mtersecte with a group of faults in the trend of EW, that is controlling the occwrence of polymetallic ore deposits.A concentric area of deposits have with obvious zoning feature of metallic elements.
出处
《矿产与地质》
1999年第5期268-273,共6页
Mineral Resources and Geology
关键词
金属矿床
成矿带
成矿亚带
元素分带
分布规律
Westsouth Liaoning
Mineralization belt
Sub mineralization belt
Concentric area of deposit
Element zoning
