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Organic matter pores in the chang 7 lacustrine shales from the Ordos Basin and its effect on reflectance measurement

引用

Petroleum Science 2023年第1期20卷 60-86页

作者： Peng Pang Hui Han Xiu-Cheng Tan Shi-Meng Ren Chen Guo Lin Xie Ling-Li Zheng Hai-Hua Zhu Yuan Gao Yun-Hui Xie School of Geoscience and Technology Southwest Petroleum UniversityChengduSichuan610500China Natural Gas Geology Key Laboratory of Sichuan Province Southwest Petroleum UniversityChengduSichuan610500China Shale Gas Industry Development Institute of Sichuan Province ChengduSichuan610500China The First Branch Mud Logging Company CNPC Bohai Drilling Engineering Co.Ltd.Tianjin300457China State Key Laboratory of Oil and Gas Reservoir Geology and Exploration Southwest Petroleum UniversityChengduSichuan610500China Beijing Center for Physical and Chemical Analysis Beijing100089China Nursing College Guizhou University of Traditional Chinese MedicineGuiyangGuizhou520002China

To quantify the pore characteristics of various macerals in Chang 7 lacustrine shales,macerals were effectively identified according to their optical and morphological characteristics,and the nanoscale pore structure of macerals was observed by scanning electron ***,the reflectances of different positions in the same pieces of vitrinite or solid bitumen with heterogeneous pores development were *** results showed that the average contents of sapropelinite,liptinite,vitrinite,inertinite and solid bitumen are 42.7%,8.7%,13.6%,13.8% and 21.2%,respectively,which suggests that the source of the organic matter of the Chang 7 shales is a mixed source *** organic pores of Chang 7 shales are enriched,and the pore shapes are mostly round or *** pore size of organic pores has a wide distribution,mainly concentrate in the range of 100-400 nm,and the average plane porosity of organic pores is 10.13%.The size order of the organic pores in various macerals is:solid bitumenfusinite>bituminite>solid bitumen>vitrinite>*** pores are mainly contributed by bituminite,solid bitumen and *** plane porosity of bituminite increases with *** the process of thermal evolution,the plane porosity of fusinite is distributed in the two ranges of 20%-28% and 1%-7%.The former is mainly the primary pores of the fusinite itself,and the latter is the secondary pores formed in the thermal *** for the organic pores of other macerals,no obvious thermal evolution law was ***,the surface imperfections of vitrinite or solid bitumen is enhanced by the enrichment of organic pores(an increase in pore size or pore number),which may result in the underestimation of their reflectances.

关键词： Ordos Basin Chang 7 member OM pore Macerals differential developmental characteristics Reflectance

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