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东准噶尔大井地区中下侏罗统沉积特征及砂岩型铀矿成矿条件分析
引用本文:鲁克改.东准噶尔大井地区中下侏罗统沉积特征及砂岩型铀矿成矿条件分析[J].新疆地质,2002,20(2):118-121.
作者姓名:鲁克改
作者单位:中国核工业地质局216大队,新疆,乌鲁木齐,830011
摘    要:分析了准尔盆地东部大井地区中下侏罗统的沉积环境、特征,发育层间氧化带的条件及铀成矿环境,认为八道湾组第一砂岩层、三工河组第一、二、三砂岩层和西山窑组第一砂岩层岩性、岩相及地球化学环境对铀矿成矿有利,发育层间氧化带并有铀矿化及异常出现,是可地浸砂岩铀矿找矿的主要目的层。

关 键 词:成矿条件  东准噶尔  沉积特征  层间氧化带  铀成矿远景  铀矿床  找矿方向
文章编号:1000-8845(2002)02-118-04
修稿时间:2002年1月7日

SEDIMENTARY FEATURES OF THE LOWER-MIDDLE JURASSIC AND CONDITIONS OF SANDSTONE-TYPE URANIUM MINERALIZATION IN EAST JUNGGAR BASIN
LU Ke-gai.SEDIMENTARY FEATURES OF THE LOWER-MIDDLE JURASSIC AND CONDITIONS OF SANDSTONE-TYPE URANIUM MINERALIZATION IN EAST JUNGGAR BASIN[J].Xinjiang Geology,2002,20(2):118-121.
Authors:LU Ke-gai
Abstract:The analysis of the sedimentary environment and features, conditions of interlayer oxidization zones' development and setting of uranium mineralization reveals that the lithology, lithofacies and geochemical environment of the 1st sandstone bed of Badaowan Formation. The 1st -3rd sandstone beds of Sangonghe Formation, and the 1st sandstone bed of Xishanyao Formation are favorable for the development of interlayer oxidization zones and uranium mineralization as well as occurrence of anomalies. These beds are the main targets for prospecting in-situ leachable sandstone-type uranium .
Keywords:East Junggar  sedimentary feature  interlayer oxidization zone  prospect of uranium mineralization
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