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鄂尔多斯盆地西缘马家滩地区石盒子组砂岩的岩石学、地球化学与成岩作用特征
引用本文:宋土顺,陶学双,刘立,王福刚,唐惠,吴文波.鄂尔多斯盆地西缘马家滩地区石盒子组砂岩的岩石学、地球化学与成岩作用特征[J].世界地质,2012,31(4):648-655.
作者姓名:宋土顺  陶学双  刘立  王福刚  唐惠  吴文波
作者单位:1. 吉林大学地球科学学院,长春130061; 2. 中国石油吉林油田公司乾安采油厂,吉林乾安131400; 3. 吉林大学环境与资源学院,长春130061; 4. 中国石油勘探开发研究院,北京100083; 5. 渤海钻探工程有限公司井下技术服务分公司,天津300283
基金项目:中国地质调查局"全国二氧化碳地质储存潜力评价与示范工程"计划项目之"二氧化碳地质储存的机理与数值模拟研究"工作项目
摘    要:鄂尔多斯盆地马家滩地区石盒子组是天然气的重点勘探层位。对马家滩地区石盒子组的岩石学特征和成岩作用研究表明,石盒子组的储层岩石类型主要为石英砂岩、岩屑石英砂岩,少量的长石岩屑砂岩。储层砂岩的成岩作用类型主要有压实和压溶、石英次生加大、胶结、溶解。根据成岩作用特征,建立了研究区储层砂岩的成岩共生序列: 自生伊利石--自生绿泥石--石英次生加大--高岭石--方解石。鄂尔多斯盆地作为中国CO2 地下埋藏的潜在目标区,开展CO2 可能埋藏层段的岩石学特征和成岩作用研究,可为CO2 地质储存的数值模拟研究提供岩石学信息。

关 键 词:石盒子组  成岩作用  马家滩地区  鄂尔多斯盆地

Sandstone petrology, geochemistry and diagenetic features of Shihezi Formation in Majiatan area, western Erdos Basin
SONG Tu-shun , TAO Xue-shuang , LIU Li , WANG Fu-gang , TANG Hui , WU Wen-bo.Sandstone petrology, geochemistry and diagenetic features of Shihezi Formation in Majiatan area, western Erdos Basin[J].World Geology,2012,31(4):648-655.
Authors:SONG Tu-shun  TAO Xue-shuang  LIU Li  WANG Fu-gang  TANG Hui  WU Wen-bo
Institution:1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. The China Jilin Oilfield Qan'an Oil Production Plant,Qan'an 131400,Jilin,China; 3. College of Environment and Resources,Jilin University,Changchun 130061,China; 4. Research Institute of Petroleum Exploration and Development,Beijing 100083,China; 5. Downhole Technology Service Company,BHDC,Tianjin 300283,China
Abstract:The Shihezi Formation is the focus point of natural exploration gas layer in Majiatan area of Ordos Basin. The research on rock characteristics and diagenesis of Shihezi Formation in the Majiatan area indicates that the stone box set of reservoir rock types are mainly quartz sandstone,lithic quartz sandstone and small amounts of feldspar-lithic sandstone. The main type of reservoir sandstone diagenetic are compaction and pressure solutionquartz overgrowth-cementation-dissolution. According to the characteristics of diagenesis and sandstone reservoir,a symbiosis of diagenetic sequence is established: authigenic illite-authigenic chlorite-quartz overgrowth-kaolinite-calcite. Ordos Basin is a CO2 buried potential target area in China. The petrological saudy on the diagenesis and buried layer section may provide information for numerical simulation of CO2geological research.
Keywords:Shihezi Formation  diagenesis  Majiatan area  Erdos Basin
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