铀矿地质Issue(z1)：247-257,11.DOI:10.3969/j.issn.10000658.2015.S1.015
鄂尔多斯盆地北东部古层间氧化带砂岩型铀矿成矿特征
Metallogenic Characteristic of the Paleo interlayer Oxidation Type Sandstone hosted Uranium Deposits in Northeastern Ordos Basin
摘要
Abstract
Northeastern Ordos basin is an important metallogenic belt for sandstone type uranium de-posits in China and is rich in uranium resources.Previous study shew that uranium deposits in the area are closely related to ancient interlayer oxidation.Previously discovered uranium deposits are located in the lower member of middle Jurassic Zhiluo formation.In region,uranium deposits are apparently controlled by ancient interlayer oxidation zone.Based on the research on uranium mineralization characteristics,the author believed that the uranium mineralization was controlled by depositional characteristics,develop-ment of the ancient interlayer oxidation zone and the direction of paleo river flow,and then established the model of alteration and uranium mineralization by the summarized ore controlling factors and urani-um mineralization characteristics.It was point out that the western regions of Daying area,Nanguo Dachengliang area and Chaidenghao area is of further prospecting potential.关键词
铀成矿特征/古层间氧化带/直罗组/鄂尔多斯盆地东北部Key words
uranium mineralization characteristics/ancient interlayer oxidation zone/Zhiluo formation/northeastern Ordos basin分类
天文与地球科学引用本文复制引用
易超,陈心路,李西得,张康,王明太,李静贤..鄂尔多斯盆地北东部古层间氧化带砂岩型铀矿成矿特征[J].铀矿地质,2015,(z1):247-257,11.基金项目
中国核工业集团公司重点科技专项“东胜基地铀资源扩大与评价技术研究”与国家高技术研究发展计划(863计划)项目(编号:2012AA061801)联合资助。 （863计划）
