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相山火山盆地组间界面、基底界面特征及其对铀矿的控制作用
引用本文:林锦荣,胡志华,谢国发,等.相山火山盆地组间界面、基底界面特征及其对铀矿的控制作用[J].铀矿地质,2014(3):135-140,167.
作者姓名:林锦荣  胡志华  谢国发  
作者单位:[1]核工业北京地质研究院、中核集团铀资源勘查与评价技术重点实验室,北京100029 [2]江西省核工业地质局261大队,江西鹰潭335001
基金项目:中核集团公司重点科技专项“相山基地铀资源扩大与评价技术研究”课题 致谢:资料收集和研究工作得到核工业270研究所、江西省核工业地质局261大队和721矿有关领导和工程技术人员的大力支持和帮助,深表谢意!
摘    要:通过对相山铀矿田钻孔资料、地球物理资料的综合研究,笔者编制了相山火山盆地火山岩组间界面、基底界面等高线图,初步查明了组间界面、基底界面形态特征和埋藏深度,认为火山岩组间界面变异部位为上部铀矿的重要赋矿空间(第1成矿空间);基底界面控制着晚期花岗斑岩,也控制着下部铀矿的空间定位(第2成矿空间).组间界面(变异部位)、基底界面与断裂构造复合处,为铀矿最有利的赋存部位.

关 键 词:相山火山盆地  火山岩组间界面  基底界面  成矿空间

The Characteristics of Interfaces between Formations and Basement in Xiangshan Volcanic Basin and their Controlls on Uranium Deposits
Institution:LIN Jin- rong, HU Zhi - hua, XIE Guo - fa, HUANG Jing - bai, RONG Jia- shu, LI Fang, WANG Yong - jian1 (1. CNNC Key Laboratory of Uranium Resource Exploration and Evaluation Technology, Beijing Research Institute of Uranium Geology, Beij ing 100029, China 2. Geological Party 261, J iangxi Nuclear Geological Bureau, Yingtan , J iangxi 335001, China)
Abstract:By means of the integrated study of boreholes and geophysical data, contour maps of inter- faces between volcanic formations and of basement have been compiled for Xiangshan volcanic basin. The morphological characteristics of interfaces and its buried depth have been preliminarily identified. Thetransformed parts of interfaces between volcanic formations are regarded as the upper ore- hosting space (called the first ore - forming space), while the interfaces of basement which controll both younger gra- nitic porphyry and the lower uranium mineralizing space (called the second ore- forming space). The best ore- forming area is located in the faults compounded with interfaces between volcanic formations and covers to basement.
Keywords:Xiangshan volcanic basin  interfaces between volcanic formations  interface of basement  ore- forming space
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