世界有色金属Issue(6)：58-61,4.
广东省惠东县伯公坑钨多金属矿区地球化学特征及找矿方向探讨
Exploration of geochemical characteristics and prospecting direction of Bogongkeng tungsten polymetallic mining area in Huidong County,Guangdong Province
柯琳 1朱沛云 1李表鹏 1卜安 1廖静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 Bogongkeng tungsten polymetallic deposit is located in the southwest section of the Lianhuashan fault zone and is a quartz vein type deposit controlled by fault structures and filled with high-temperature hydrothermal fractures after the magmatic period.Mineralization occurs in the contact zone between the Late Cretaceous fine-grained(speckled)biotite diorite granite controlled by faults and the Jurassic Yinpingshan Formation.Mineralization occurs in secondary faults and fractures that control the mineralization faults,and is an important direction for prospecting in areas with rock alteration such as silicification,dolomitization,electrochemicalization,pyrite mineralization,and fluoritization.关键词
钨多金属矿/地球化学/找矿方向/莲花山断裂带/广东省Key words
tungsten 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
柯琳,朱沛云,李表鹏,卜安,廖静..广东省惠东县伯公坑钨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,2025,(6):58-61,4.
