首页|桂西龙田孤立台地边缘金矿地质特征及找矿方向

桂西龙田孤立台地边缘金矿地质特征及找矿方向

扫码查看
龙田孤立碳酸盐岩台地地处右江盆地腹地,沿台地边缘1km范围已发现3处小型金矿,成矿地质条件优越.本文总结了龙田台地边缘金矿的矿床地质特征和主要控矿因素,对金矿的成矿物质来源和成矿时代进行了探讨.研究表明,金矿主要分布于龙田环台断裂的次级断裂带内,成矿物质来源主要为围岩三叠系,成矿流体以大气降水为主.金矿总体形成于印支晚期—燕山早期,此时右江盆地正处于碰撞挤压到拉伸的构造转换期.
Geological characteristics and prospecting direction of gold deposits on the Longtian isolated platform margin in western Guangxi
The Longtian isolated carbonate platform is located in the hinterland of the Youjiang Basin.Three small gold deposits have been discovered within a 1km range along the platform margin,and the geological conditions for mineralization are superior.This article summarizes the geological characteristics and main controlling factors of the gold deposit on the margin of the Longtian Platform,and explores the source of ore-forming materials and ore-forming era of the gold deposit.Research has shown that gold deposits are mainly distributed within the secondary fault zone of the Longtian Huantai Fault,with the main source of ore-forming materials being the Triassic surrounding rock,and the ore-forming fluid mainly being atmospheric precipitation.The gold deposits were generally formed in the late Indosinian to early Yanshanian periods,during which the Youjiang Basin was in a tectonic transition period from collision compression to stretching.

Western GuangxiGold Oresthe Isolated carbonate platformExploration direction

王学恒、李玉坤、梁国科、黄健、唐维

展开 >

广西壮族自治区地质调查院,广西 南宁 530023

桂西 金矿 孤立碳酸盐岩台地 找矿方向

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(7)