文章摘要
鄂尔多斯盆地北部煤系非常规天然气 成藏特征—以U-1井为例
  
DOI:
中文关键词: 鄂尔多斯盆地北部  含煤地层  非常规天然气  成藏特征  气体同位素
英文关键词: 
基金项目:中国矿业大学煤层气资源与成藏过程教育部重点实验室开放基金(2015-06);山西省煤基重点科技攻关项目(MQ2014-02)
作者单位
姚海鹏1,2,朱炎铭1,刘刚1 1.中国矿业大学 煤层气资源与成藏过程教育部重点实验室江苏 徐州 221116.内蒙古自治区煤田地质局内蒙古 呼和浩特 010010 
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中文摘要:
      石炭-二叠纪含煤地层是鄂尔多斯盆地煤层气、页岩气和致密砂岩气叠合成藏的主要层位.3种气藏均属于热成因气藏,但成藏特征存在差异,依据大量的钻井、测井资料对3种气藏的平面展布特征进行了探讨,并选择具有代表性的U-1井以山西组下段和太原组为目标层位,从垂向上对3种气藏的地球化学、储层物性、含气性、气体同位素测试数据进行了剖析,结果表明:研究区页岩及煤层有机碳含量高,有机质类型均为Ⅲ型,处于高成熟-过成熟阶段,累计总生烃量154 mg/g.在孔隙度方面致密砂岩储层>煤储层>页岩储层,储层孔隙主要由纳米孔组成,结构不规则且形态呈开放状态.在渗透性方面致密砂岩较好,煤储层次之,页岩较差.在含气性方面煤储层>砂岩储层>页岩储层.在研究区太原组至山西组下段主要形成了煤层气、页岩气与致密砂岩气的复合型气藏.
英文摘要:
      In Ordos Basin, coal-bearing strata of Carboniferous-Permian are the main layer for coalbed methane, shale gas and tight sand gas stacked accumulation. Three kinds of gas reservoirs belong to thermal genetic gas reservoir, but their reservoir characteristics are different. On the basis of a large number of drilling and logging data, the plane distribution characteristics were discussed that of three kinds of gas reservoirs, Taiyuan Formation and low of Shanxi Formation of U-1 well was selected, which is representative, as the destination layer. The data of geochemistry, reservoir properties, gas content and gas isotope from vertical were analyzed. The results show that shale and coal seam have high organic content ,which is mainly for type Ⅲ kerogen and in high mature and over mature stage. The total quantity of hydrocarbon in organic matter is 154 mg/g. In terms of porosity, tight sandstone reservoir is higher than coal reservoir and shale reservoir, and shale reservoir is lowest. The reservoir porosity is mainly composed of nano pores, which have irregular structure and are open. Tight sandstone in permeability is better than coal seam and shale, and shale is poor. In terms of gas bearing, coal reservoir is higher than tight sandstone reservoir and shale reservoir, and shale reservoir is lowest. In the study area Taiyuan Formation to the low of Shanxi Formation mainly formed the composite gas reservoirs of coalbed methane, shale gas and tight sandstone gas.
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