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松辽盆地东南部铀矿找矿目的层原生地球化学类型与后生蚀变作用
引用本文:林锦荣,田华,董文明,夏毓亮,郑纪伟,戚大能,腰善丛.松辽盆地东南部铀矿找矿目的层原生地球化学类型与后生蚀变作用[J].铀矿地质,2009,25(4):202-207.
作者姓名:林锦荣  田华  董文明  夏毓亮  郑纪伟  戚大能  腰善丛
作者单位:1. 核工业北京地质研究院,北京,100029
2. 辽河石油勘探局,辽宁,盘锦,124010
摘    要:通过对松辽盆地东南部区域地质资料综合分析及铀资源区域钻探评价,基本查明了目的层泉头组、姚家组、四方台组岩相古地理、岩性与砂体特征。通过对目的层岩石形成的地球化学环境研究,识别和划分了原生地球化学类型和后生蚀变作用类型,原生地球化学类型有原生氧化和原生还原类型,后生蚀变作用类型有油气、煤层气还原作用和后生氧化作用类型。对比研究了原生地球化学类型及后生蚀变作用类型岩石、矿物及化学成分特征,提出了油气、煤层气还原后生蚀变作用识别标志。认为原生含炭质砂岩铀有强烈的沉积预富集,油气、煤层气还原作用中有铀的叠加富集。

关 键 词:原生地球化学  后生蚀变作用  油气  煤层气还原作用

Original geochemical types and epigenetic alteration of rocks in prospecting target stratum for uranium deposit in the southeast of Songliao basin
LIN Jin-rong,TIAN Hun,DONG Wen-ming,XIA Yu-liang,ZHENG Ji-wei,QI Da-neng,YAO Shan-cong.Original geochemical types and epigenetic alteration of rocks in prospecting target stratum for uranium deposit in the southeast of Songliao basin[J].Uranium Geology,2009,25(4):202-207.
Authors:LIN Jin-rong  TIAN Hun  DONG Wen-ming  XIA Yu-liang  ZHENG Ji-wei  QI Da-neng  YAO Shan-cong
Institution:LIN Jin-rong , TIAN Hua , DONG Wen-ming, XIA Yu-liang, ZHENG Ji-wei , QI Da-neng , YAO Shan-cong (1. Beijing Research Institute of Uranium Geology, Beijing 100029, China ; 2. Tongliao Uranium Mine Liaohe Bureau of Petroleum Exploration and Development, Panjin, Liaoning 124010, China)
Abstract:By comprehensive analysis on informations of regional geology and evaluating drillhole works of uranium resources in the southeast of Songliao basin, lithofacies-palaeogeography features, lithologies and sandbody characteristics of target layes in Quantou formation , Yaojia formation and Sifangtai formation have been basically found out. By research on geochemical environment of rocks in target layez, types of original geochemistry and epigenetic alteration have been identified and classified. The types of original geochemistry have been divided into types of original oxidation and original reduction, and the types of epigenetic alteration have been divided into types of reduction by oil-gas and coalbed gas and epigenetic oxidation. By comparative study on mineral and chemical characteristics of original geochemistry and epigenetic oxidation, identification marks for oil-gas and coalbed gas reduced epigenetic oxidation have been proposed. It is proposed that uranium was strongly pre-concentrated in original sandstone that bearing carboniferous matter, and reduction by oil-gas and coalbed gas made uranium superimpose and concentrate in alterated rocks.
Keywords:original geochemistry  epigenetic alteration  reduction by oil-gas and coalbed gas
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