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黄陵地区中生代含煤岩系油气与铀成矿的耦合关系
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  • 英文篇名:Coupling relationship between oil and gas of Mesozoic coal-bearing measures and uranium metallogenesis in Huangling area
  • 作者:司庆红 ; 曹惠锋 ; 李建国 ; 司马献章 ; 俞礽安 ; 刘厚宁 ; 刘晓雪 ; 张超
  • 英文作者:SI Qinghong;CAO Huifeng;LI Jianguo;SIMA Xianzhang;YU Reng'an;LIU Houning;LIU Xiaoxue;ZHANG Chao;Tianjin Center,China Geological Survey;Geological Survey Institude of China Nuclear Industry Group Co.Ltd.;
  • 关键词:黄陵地区 ; 中生代 ; 含煤岩系 ; 油气(藏) ; 铀矿(点) ; 烃类流体 ; 铀伴生蚀变矿物
  • 英文关键词:Huangling area;;Mesozoic;;coal-bearing measures;;oil-gas reservoir;;uranium deposits(points);;hydrocarbon-bearing fluids;;uranium-associated altered minerals
  • 中文刊名:煤田地质与勘探
  • 英文刊名:Coal Geology & Exploration
  • 机构:中国地质调查局天津地质调查中心;中陕核工业集团地质调查院有限公司;
  • 出版日期:2019-02-25
  • 出版单位:煤田地质与勘探
  • 年:2019
  • 期:01
  • 基金:国家重点研发计划项目(2018YFC0604200);; 国家重点基础研究发展计划(973计划)项目(2015CB453000);; 中国地质调查局地质调查项目(DD20160127)~~
  • 语种:中文;
  • 页:19-25+35
  • 页数:8
  • CN:61-1155/P
  • ISSN:1001-1986
  • 分类号:P618.13;P619.14
摘要
为了明确黄陵地区中生代含煤岩系油气与铀成矿的耦合关系,进行了钻孔与剖面的野外地质调查、钻孔资料与实验数据的分析与处理、油气藏与铀矿(点)信息的综合整理,系统研究了中生代含煤岩系构造–沉积体系、铀矿地质特征和油气地质特征,从油气藏与铀矿(点)的空间分布关系、含烃流体与铀的伴生蚀变矿物的成因关系以及烃源岩生烃与铀成矿的时间关系展开讨论。研究表明:中生代含煤岩系铀矿(点)多分布在基岩剥蚀边界或小型断裂附近,且水平投影位于油气有利相带周缘;烃类流体组分及煤层气的中间产物可能参与氧化还原反应,生成黄铁矿、方解石等与铀矿物具有密切伴生关系的矿物;中生代含煤岩系烃源岩主生烃期和排烃期总体早于铀矿主成矿期,烃类流体可能通过运移影响铀成矿作用。
        In order to clarify the coupling relationship between oil and gas of Mesozoic coal-bearing measures(reservoir)and uranium deposits(points) in Huangling area, field geology investigations of boreholes and sections, analysis and processing of borehole data and experimental data, and integration of reservoir and uranium(point) information were carried out.Collation and systematic study of tectonic-sedimentary systems of Mesozoic coal-bearing mesure, uranium geological characteristics, oil and gas geology characteristics, spatial distribution relationship between hydrocarbon reservoirs and uranium deposits, genetic relationship between hydrocarbon-bearing fluids and uranium-associated altered minerals, and the time relationship between hydrocarbons and uranium mineralization were discussed. The study shows that the uranium deposits of Mesozoic coal-bearing(spots) measures were mostly distributed near the boundary of the bedrock erosion or small faults, and the horizontal projection is located at the periphery of the favorable oil and gas facies belt. The hydrocarbon fluid components and the intermediate products of the coalbed gas may have participated in the re-dox reactions, then the uranium associated altered minerals such as pyrite, clay minerals, and calcite have been produced. The main hydrocarbon generation period of Mesozoic coal-bearing source rocks was overall earlier than the main miner-alization period of uranium deposits, and hydrocarbon fluids may have migration time conditions that affected uranium mineralization.
引文
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