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粤北佛冈岩体琶江地区断裂构造特征与找矿方向

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粤北佛冈复式岩体中部琶江地区断裂构造发育,主要有近东西向、北东向、北西向、北北西向及近南北向五组.文章对这五组断裂构造进行了野外调查及室内综合研究分析,将区内断裂构造划分为三级,一级断裂为近东西向社岗-门楼富断裂、竹园-草子顶断裂;二级断裂为北东向仙人石断裂、汤塘断裂;三级断裂为北东向次级断裂、北西向、北北西向及近南北向断裂.其中近东西向、北东向断裂为压扭性断裂,控制了区内铀矿床、铀矿点的分布与产出,为重要的控岩控矿断裂;北北西向17号带、近南北向5号、83号带、F1-1断裂带为主要含矿构造,次级北东向2号带、F1 断裂带为次要含矿断裂.综合分析认为区内北北西向17号带、近南北向5号、83号带、F1-1断裂带为下一步重点工程揭露部位.
Fault Characteristics and Uranium Prospecting Direction in Pajiang Area of Fogang Pluton in Northern Guangdong
The fault structure in Pajiang area of the central Fogang complex pluton in northern Guangdong province is mainly divided into five groups:nearly east-west,northeast,north west,north northeast,north north west and nearly south-north.The paper conducted field survey and indoor comprehensive analysis of the five groups of fault structures,and divided the fault structure in the area into three levels:the first level faults are nearly east-west Shegang-Menloufu fault and Zhuyuan-Caoziding fault;the second level faults are northeast Xianrenshi fault and Tangtang fault;the third level faults are northeast,northewest,north north west and nearly south-north.Among them,the nearly east-west and northeast faults are compression-torsion faults,which control the distribution and output of uranium deposits and occurrences in the area,and are important rock-control and ore-control faults;the north north-west No.17 fault,nearly south-north No.5,No.83 and F1-1 faults are tensile-torsion faults,which are the main ore-bearing structures,and the secondary north east No.2,F1 faults is a minor ore-bearing fault.The comprehensive analysis shows that the north north-west No.17 fault and nearly south-north No.5,No.83 and F1-1 faults in the area are the key expose target of the next project.

Pajiang areaore-controlling faultore-bearing faultprospecting direction

许丽丽

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核工业二九〇研究所,广东 韶关 512029

琶江地区 控矿断裂 含矿断裂 找矿方向

中国核工业地质局铀矿调查与科研项目中国核工业地质局铀矿调查与科研项目中国核工业地质局铀矿调查与科研项目广东省科技专项基金项目

202140202241-3202241-4201112166271152

2024

铀矿地质
中国核学会铀矿地质学会

铀矿地质

CSTPCD
影响因子:0.714
ISSN:1000-0658
年,卷(期):2024.40(3)
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