世界有色金属Issue(14)：68-70,3.
广东省惠东县元坑钨锡多金属矿区地球化学特征及找矿方向探讨
Geochemical characteristics and exploration direction of the Yuankeng Tungsten Tin polymetallic mining area in Huidong County,Guangdong Province
廖静 1赵新胤 1郭丽荣 1朱沛云 1王长全1
作者信息
- 1. 广东省有色金属地质局九三一队,广东 汕头 515041
- 折叠
摘要
Abstract
The Yuankeng tungsten tin polymetallic mining area is located in the northern part of the Zuokeng area,in the eastern part of the Wuyi metallogenic belt in Guangdong Province,sandwiched by the Zijin Boluo fault and the western belt of the Lianhuashan fault zone.This area is a magmatic hydrothermal filled metasomatic deposit controlled by fault structures.The ore body is located in the shallow tidal flat sandstone of the Lower Jurassic Qingkeng Formation near the contact zone with the rock mass and has been altered by fault structures.The northeast and northwest trending fault structures have important prospecting directions,such as silicification,ceratopsization,and chloritization.关键词
钨锡多金属矿/地球化学/找矿方向/莲花山断裂带/广东省Key words
tungsten tin polymetallic ore/Geochemistry/Direction of mineral exploration/Lianhua Mountain Fault Zone/Guangdong Province分类
天文与地球科学引用本文复制引用
廖静,赵新胤,郭丽荣,朱沛云,王长全..广东省惠东县元坑钨锡多金属矿区地球化学特征及找矿方向探讨[J].世界有色金属,2024,(14):68-70,3.
