摘要
阐述了新兴县天露山地区矿山地质特征,分析了其成矿地质条件,总结了其找矿标志。对天露山地区的找矿潜力进行了初步的评价。天露山地区历史上岩浆活动频繁,岩浆侵入多期多次,岩浆活动为该区成矿带来了较好的来源。构造活动亦呈多期多次,往往叠加,形成不同力学性质,充填各种成份复杂蚀变构造岩的断裂带,这些断裂构造提供了良好的成矿元素运移和活化通道,同时亦提供了沉淀富集空间,所以该区内矿物的成矿地质条件是比较有利的。
The geological characteristics of mines in Tianlushan area in Xinxing County are described,the geological conditions of mineralization are analyzed,and the signs of prospecting are summarized.A preliminary evaluation of the prospecting potential of the Tianlushan area has been carried out.In the history of Tianlushan area,magmatic activity was frequent,and magma invaded many times,and magmatic activity brought a good source of mineralization in this area.The tectonic activity also presents multiple phases,often superimposed,forming fault zones with different mechanical properties,filling various complex altered tectonic rocks.These fault structures provide a good channel for the migration and activation of ore-forming elements,as well as Precipitation enrichment space,so the mineralization geological conditions of the minerals in this area are more favorable.
作者
王云华
WANG Yun-hua(The 293rd team of Guangdong Nuclear Industry Geology Bureau,Guangzhou 510000,China)
出处
《世界有色金属》
2020年第17期54-55,共2页
World Nonferrous Metals
关键词
新兴县天露山地区
成矿地质条件
找矿潜力
tianlushan area,Xinxing County
metallogenic geological conditions
prospecting potential
