天然气地球科学

• 天然气地质学 • 上一篇    下一篇

重庆地区五峰组—龙马溪组页岩笔石光学特征及其在成熟度评价中的应用

罗情勇,郝婧玥,李可文,戴娜,栾进华,程礼军,张志平,胡科,钟宁宁   

  1. 1.中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249;
    2.重庆地质与矿产研究院,重庆 400042;
    3.广东省企业自主创新促进会,广东 广州 510060
  • 收稿日期:2017-04-01 修回日期:2017-09-07 出版日期:2017-12-10 发布日期:2017-12-10
  • 通讯作者: 钟宁宁(1960-),男,广东佛冈人,教授,博士.主要从事有机岩石学与油气地球化学研究. E-mail:nnzhongxp@cup.edu.cn.
  • 作者简介:罗情勇(1987-),男,江西高安人,副教授,博士.主要从事有机岩石学与油气地球化学研究.E-mail:qingyong.luo@cup.edu.cn.
  • 基金资助:

    国家自然科学基金(编号:41503028);国家科技重大专项(编号:2016ZX05034003-001);中国石油大学(北京)科研基金(编号:2462014YJRC022;2462015YQ0107)联合资助.

The optical characteristics of the graptolites in the Wufeng-LongmaxiFormations and its application for the thermal maturity evaluation

Luo Qing-yong,Hao Jing-yue,Li Ke-wen,Dai Na,Luan Jin-hua,Cheng Li-jun,Zhang Zhi-ping,Hu Ke,Zhong Ning-ning   

  1. 1.State Key Laboratory of Petroleum Resources and Prospecting,China University of Petroleum,Beijing 102249,China;
    2.Chongqing Institute of Geology & Mineral Resources,Chongqing 400042,China;
    3.Guangdong Promotion Association of Enterprise Innovation,Guangzhou 510060,China
  • Received:2017-04-01 Revised:2017-09-07 Online:2017-12-10 Published:2017-12-10

摘要:

上奥陶统五峰组—下志留统龙马溪组富有机质页岩以富含笔石为特征,是中国上扬子地区最重要的烃源岩层和页岩气储层之一,但在实际工作中却存在成熟度难以确定的困难。通过对重庆地区五峰组—龙马溪组大量块光片中笔石的光学特征观察和反射率测试,结果表明:五峰组—龙马溪组页岩中被认为是类镜质组颗粒或者沥青的有机质可能是笔石表皮体。五峰组—龙马溪组页岩有机质的非颗粒状结构笔石表皮体丰度较大,且其具有不同于沥青的特殊生物结构和光学特征:生物结构复杂、分节、具有纺锤层、易被黄铁矿充填,尤其是在高过成熟阶段表现出强烈的各向异性。五峰组—龙马溪组样品中非颗粒状结构笔石表皮体的平均双反射率值(最大反射率与最小反射率之差)介于0.71%~5.78%之间,其光学性质类似于二轴光性体。非颗粒状结构笔石表皮体的最大反射率经校正后,渝东南地区五峰组—龙马溪组的等效镜质体反射率值介于2.75%~4.72%之间;而渝东北城口和巫溪地区五峰组—龙马溪组的等效镜质体反射率值分别为1.05%~1.17%和5.42%~5.58%。渝东北巫溪和渝东南五峰组—龙马溪组样品处于过成熟热演化阶段,而渝东北城口五峰组—龙马溪组样品仍处于成熟热演化阶段。

关键词: 笔石有机质, 光学性质, 热成熟度, 五峰组&mdash, 龙马溪组, 重庆地区

Abstract:

The organic-rich shale of Wufeng-Longmaxi Formations (Ordovician-Silurian) is one of the most important hydrocarbon source rocks and shale gas reservoirs in the upper Yangtze region of China.They contain abundant graptolites and the determination of their thermal maturity has always been a difficult problem.Based on the observation of abundant polished blocks,the graptolites were easily mistaken for vitrinite-like particles or bitumen.Abundant non-granular graptolites were observed in these sediments.Their biological and optical characteristics,which are different from bitumen or vitrinite-like particles,include complex and segmented structure,fusellar layers,abundant in-fill pyrites and strong anisotropy at the high-post mature stages.The bireflectance (Rmax-Rmin) values of the non-granular graptolites fall between 0.71% and 5.78%,indicating its behaviour similar to the optical biaxial material.The equivalent vitrinite reflectance values (EqVRO),calculated from the mean maximum reflectance of non-granular graptolite,fall in the range of 2.75%-4.72%,1.05%-1.17% and 5.42%-5.58% for the studied samples from the southeastern Chongqing,Chengkou and Wuxi of northeastern Chongqing,respectively,indicating that the thermal maturity of the samples from southeastern Chongqing and Wuxi area is postmature,whereas the thermal maturity of the samples from Chengkou area is mature.

Key words: Graptolite, Optical characteristics, Thermal maturity, Wufeng-Longmaxi Formations, Chongqing area

中图分类号: 

  • TE122.1+13


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