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层间氧化带砂岩型铀矿的形成条件及找矿判据
引用本文:黄世杰.层间氧化带砂岩型铀矿的形成条件及找矿判据[J].铀矿地质,1994,10(1):6-13.
作者姓名:黄世杰
作者单位:核工业总公司地质局
摘    要:本文综合分析了国内外层间氧化带砂岩型铀矿形成的大地构造背景和盆地结构构造,岩相古地理,地貌与气候,水动力与水学,层间氧化带发育等必备的有利条件,并进而提出了铀源丰富,气候干旱;稳定大盆,产状平缓,深积大扇,相变不大;砂泥互层,埋深不大;含水性好,透水性强;层间氧化带发育,富含还原剂等找矿判据,以及“六位一体”的水成成矿模式。

关 键 词:铀矿床  砂岩型  成矿条件  找矿

FORMATION CONDITIONS AND PROSPECTING CRITERIA FOR SANDSTONE URANIUM DEPOSIT OF INTERLAYERED OXIDATION TYPE
Huang Shijie.FORMATION CONDITIONS AND PROSPECTING CRITERIA FOR SANDSTONE URANIUM DEPOSIT OF INTERLAYERED OXIDATION TYPE[J].Uranium Geology,1994,10(1):6-13.
Authors:Huang Shijie
Abstract:This paper comprehensively analyses the geotectonic setting and favourable conditions,such as structure of the basin, sedimentary factes and paleogeography, geomorphology andclimate, hydrodynamics and hydrogeochemistry, the development of interlayered oxidationetc,necessary for the formation of sandstone uranium deposit of interlayered oxidation type,and further proposes the following prospecting criteria, namely: abundant uranium source,arid climate,stable big basin, flat-lying sandstone bed, big alluvial fan,little change in sedimentary facies,intercalation of sandstone and mudstone beds, shallow burying of sandstonebed, well-aquiferous sandstone bed,high permeability of sandstone bed,development of interlayered oxidation,and high content of reductant in sandstone. In addition, the 6 in 1 hydrogenic genetic model is proposed.
Keywords:Formation condition  Prospecting criteria  Genetic model
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