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下古生界有机质成熟度评价新参数:笔石表皮体光学特征再研究
引用本文:罗情勇,郝婧玥,李可文,徐耀辉,王晓梅,王华建,栾进华,胡科,李甜,钟宁宁.下古生界有机质成熟度评价新参数:笔石表皮体光学特征再研究[J].地质学报,2019,93(9):2362-2371.
作者姓名:罗情勇  郝婧玥  李可文  徐耀辉  王晓梅  王华建  栾进华  胡科  李甜  钟宁宁
作者单位: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;中国石油大学(北京)地球科学学院,北京,102249;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;广东省企业自主创新促进会,广州,510060;长江大学油气资源与勘探技术教育部重点实验室,武汉,430100;中国石油勘探开发研究院,北京,100083;重庆地质矿产研究院,重庆,400042
基金项目:本文为国家自然科学基金项目(编号41503028)、中国石油天然气股份有限公司科学研究与技术开发课题(编号2016A- 0204)和国家油气重大专项(编号2016ZX05034003- 001)资助成果。
摘    要:下古生界缺失高等植物来源的镜质组,其有机质成熟度的确定一直是油气源岩评价的难题之一。基于对含笔石页岩的反射光显微镜观察和低成熟度含笔石页岩与煤共置的热压模拟实验,研究了下古生界海相页岩笔石表皮体的光性特征及其热演化规律,探讨了笔石表皮体随机反射率作为有机质热演化参数的可行性。下古生界海相页岩非粒状笔石表皮体呈条带状顺层或者碎片状产出、颗粒较大,光学特征类似于镜质组,适合于测量反射率。非粒状笔石表皮体随机反射率■换算为等效镜质组反射率■的关系式为■。采用笔石表皮体随机反射率分析了上扬子地区东部五峰组—龙马溪组页岩的有机质成熟度分布特征,认为非粒状笔石表皮体随机反射率是一个实用的下古生界烃源岩有机质成熟度指标,为确定下古生界有机质成熟度提供了一种可信的解决方案。

关 键 词:下古生界  有机质成熟度  热演化参数  反射率  笔石表皮体  五峰组-龙马溪组
收稿时间:2019/1/8 0:00:00
修稿时间:2019/5/28 0:00:00

A new parameter for the thermal maturity assessment of organic matter from the Lower Palaeozoic sediments: a re study on the optical characteristics of graptolite periderms
LUO Qingyong,HAO Jingyue,LI Kewen,XU Yaohui,WANG Xiaomei,WANG Huajian,LUAN Jinhu,HU Ke,LI Tian and ZHONG Ningning.A new parameter for the thermal maturity assessment of organic matter from the Lower Palaeozoic sediments: a re study on the optical characteristics of graptolite periderms[J].Acta Geologica Sinica,2019,93(9):2362-2371.
Authors:LUO Qingyong  HAO Jingyue  LI Kewen  XU Yaohui  WANG Xiaomei  WANG Huajian  LUAN Jinhu  HU Ke  LI Tian and ZHONG Ningning
Institution:1) State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249; 2) College of Geoscience, China University of Petroleum (Beijing), Beijing, 102249,1) State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249; 2) College of Geoscience, China University of Petroleum (Beijing), Beijing, 102249,1) State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249;3) Guangdong Promotion Association of Enterprise Innovation, Guangzhou, 510060,4) Key Laboratory of Exploration Technologies for Oil and Gas Resources (Yangtze University), Ministry of Education, Wuhan, 430100,5) Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing, 100083,5) Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing, 100083,6) Chongqing Institute of Geology & Mineral Resources, Chongqing, 400042,6) Chongqing Institute of Geology & Mineral Resources, Chongqing, 400042,6) Chongqing Institute of Geology & Mineral Resources, Chongqing, 400042 and 1) State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum (Beijing), Beijing, 102249; 2) College of Geoscience, China University of Petroleum (Beijing), Beijing, 102249
Abstract:
Keywords:Lower Paleozoic  thermal maturity  thermal evolution parameter  reflectance  graptolite periderm  Wufeng- Longmaxi formations
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