节点文献

鄂尔多斯盆地中部气田马五段气源岩地球化学特征

GEOCHEMICAL CHARACTERISTICS OF O 1m 5 GAS SOURCE ROCKS IN CENTRE GAS FIELD IN EERDUOSI BASIN

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 李景贵张谦崔明中张中宁程学惠

【Author】 Li Jinggui,Zhang Qian,Cui Mingzhong,Zhang Zhongning and Cheng Xuehui(Lanzhou Institute of Geology,Academia Sinica).

【机构】 中国科学院兰州地质研究所

【摘要】 马五段是鄂尔多斯盆地中部气田下奥陶统主力气源岩中的主力生烃层段。通过对比4口井23个样品下奥陶统马五段气源岩氯仿沥青“A”、氯仿沥青“C”含量,族组成及饱和烃馏分生成物标记化合物地化特征,认为该段气源岩氯仿沥青“A”和氯仿沥青“C”具同源性,但前者成熟度略高于后者,前者含量及其总烃含量随样品有机碳值增高而增大;相反,后者含量及其总烃含量随样品有机碳值增大而减小;二者的沥青转化率和烃转化率都随TOC值增大而变小。根据二者含量、总烃含量以及沥青转化率和烃转化率与样品有机碳关系的综合研究,提出马五段碳酸盐岩气源岩有机碳含量下限值可确定为0.04%。最后认为,评价高、过成熟阶段碳酸盐岩大中型气田气源岩不仅要依据有机质丰度的高低,氯仿沥青“A”的数量和质量,还必须考虑到氯仿沥青“C”的数量和质量,此外还要结合沥青转化率和烃转化率加以综合判识。

【Abstract】  1m 5(i.e.the fifth member of Majiagou Formation,Lower Ordovician)is the major hydrocarbon source interval in the major gas source rocks of the Lower Ordovician in Centre gas field in Eerduosi Basin.Through contrasting the chloroform bitumen “A” content,chloroform bitumen “C” content and group composition,and the geochemical characteristics of saturated hydrocarbon distillate labeled compound in 23 samples from O 1m 5 gas source rocks in 4 wells,it is thought that the chloroform bitument “A” and choloroform bitument “C” of the gas source rocks in the interval are of consanguineous property,however the maturity of the former is higher than that of the latter,and the former′s content and its total hydrocarbon content increase with the raise of organic carbon content in the samples;on the contrary,the latter′s content and its total hydrocarbon content decrease in the same case;and that the bitumen and hydrocarbon conversion rates of the two decrease with the increase of total organic carbon value.According to a comprehensive research on the relations of the choloroform bitumen “A” content,choloroform bitumen “C” content,total hydrocarbon content,bitumen conversion rate and hydrocarbon conversion rate with the organic carbon content in the samples,it is proposed that the cutoff of the organic carbon content in the gas source rock of O 1m 5 carbonate rock may be determined as 0.04%.Finally,it is thought that not only the size of organic matter abundance and the quantity and quality of choloroform bitumen “A”,but also those of choloroform bitumen “C” must be all considered in evaluating the gas source rocks in large and medium sized gas fields of high and post maturity carbonate rocks.In addition,a comprehensive judgement must be also carried out in combination with the bitumen and hydrocarbon conversion rates.

  • 【文献出处】 天然气工业 ,NATURAL GAS INDUSTRY , 编辑部邮箱 ,1998年05期
  • 【分类号】P618.13
  • 【被引频次】6
  • 【下载频次】201
节点文献中: 

本文链接的文献网络图示:

本文的引文网络