摘要
塌山-江西坑位于武夷成矿带粤东段,北东向莲花山深断裂带中段,莲花山整装勘查区中部,属莲花山锡铜多金属成矿带的核心区域。该区具有优越的成矿地质条件,其化探异常规模大,浓集中心明显,区内整体工作程度较低,已知矿床外围及深部具有较好的找矿潜力。
Tashan-Jiangxi Keng is located in the eastern part of the Wuyi metallogenic belt,the middle section of the Lianhuashan deep fault zone from the northeast and the central part of the Lianhuashan self-contained exploration area.It is the core area of the Lianhuashan tin-copper polymetallic metallogenic belt.This area has excellent ore-forming geological conditions,its geochemical prospecting anomaly is large in scale,its concentration center is obvious and the overall work in the area is relatively low.It is known that the periphery and deep part of the deposit have good prospecting potential.
作者
张帅帅
朱沛云
ZHANG Shuai-shuai;ZHU Pei-yun(Nonferrous Metals Geological Bureau Of Guangdong Province 931 Battalion,Shantou 515041,China)
出处
《世界有色金属》
2021年第20期67-69,共3页
World Nonferrous Metals
关键词
锡多金属矿
地质特征
找矿前景
塌山-江西坑
广东省
tin polymetallic ore
Geological characteristics
Prospecting prospect
Collapse mountain-Jiangxi pit
Guangdong Province