Characteristics of the mud shale reservoirs in coal-bearing strata and resources evaluation in the eastern margin of the Ordos Basin, China

Author:

Chen Yue12ORCID,Ma Dongmin13,Xia Yucheng1,Guo Chen12ORCID,Yang Fu123,Shao Kai24

Affiliation:

1. College of Geology and Environment, Xi’an University of Science and Technology, Xi’an, China

2. Post-doctorate R&D Base of Geological Resources and Geological Engineering, Xi’an University of Science and Technology, Xi’an, China

3. Key Laboratory of Coal Resources Exploration and Comprehensive Utilization, Ministry of Land and Resources, Xi’an, China

4. Shaanxi Coalbed Methane Development Co., Ltd, Xi’an, China

Abstract

As the co-exploration and co-production of unconventional gas have become a new trend of the unconventional gas exploration and development in the eastern margin of the Ordos Basin, this study focuses on the distribution, pore characteristics, geochemical properties, and mineral composition of the mud shale in the coal-bearing strata. The results show that the mud shale in the coal-bearing strata is distributed relatively stably with an average cumulative thickness of 77.60 m and a buried depth of 200–2400 m, increasing from east to west. The total organic carbon content of mud shale is relatively high, ranging from 0.14% to 39.9%, and the thermal maturity ranges from 0.23% to 2.49%, affected by both buried depth and magmatic intrusion. The organic matter type of the mud shale is dominated by type III, favorable for gas generation. The mineral composition of mud shale is mainly clay minerals and quartz, with low brittle minerals content (averaging 30.34%) and high kaolinite content (averaging 59.23%). Pores and micro-fissures are relatively developed in the mud shale, dominated by intergranular pores, organic pores, and the micro-fissures developed between brittle mineral crystals, within crystals and between clay mineral particles, with a porosity of 1.05%–1.59% and a permeability of 0.001–0.142 (×10−3µm2). The specific surface area of pores in mud shale is 12.31–28.99 m2/g, and the total pore volume is 0.0146–0.0483 cm3/g. Mesopores and micropores (mainly slit shaped pores) provide the main pore volume of mud shale, and micropores contribute most of the specific surface area. The controlling factors on pore development include the total organic carbon, thermal maturity, and inorganic minerals composition. The total amount of shale gas resources is 2.49 × 1012 m3, and the Linxian-Xingxian area and Shilou-Daning area are the potential favorable zones for shale gas exploration and development.

Funder

Projects Funded by China Postdoctoral Science Foundation

Doctoral Research Starting Foundation of Xi’an University of Science and Technology

Ministry of Land and Resources of the People’s Republic of China' Special Funds for Scientific Research on Public Causes

Research Projects of the Geological Research Institute for Coal Green Mining of Xi’an University of Science and Technology

Major National Science and Technology Special Projects

Independent Projects of the Key Lab. of Coal Resources Exploration and Comprehensive Utilization of Ministry of Land and Resources of China

Natural Science Foundation Research Projects of Shaanxi Province

Publisher

SAGE Publications

Subject

Energy Engineering and Power Technology,Fuel Technology,Nuclear Energy and Engineering,Renewable Energy, Sustainability and the Environment

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