气候变化领域集成服务门户(CCPortal): Friction of Longmaxi Shale Gouges and Implications for Seismicity During Hydraulic Fracturing

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DOI	10.1029/2020JB019885
	Friction of Longmaxi Shale Gouges and Implications for Seismicity During Hydraulic Fracturing
	An M.; Zhang F.; Elsworth D.; Xu Z.; Chen Z.; Zhang L.
发表日期	2020
ISSN	21699313
卷号	125 期号:8
英文摘要	Longmaxi formation shales are the major target reservoir for shale gas extraction in Sichuan Basin, southwest China. Swarms of earthquakes accompanying hydraulic fracturing are observed at depths typifying the Longmaxi formation. Mineral composition varies broadly through the stratigraphic section due to different depositional environments. The section is generally tectosilicate-poor and phyllosilicate-rich with a minor portion the converse. We measure the frictional and stability properties of shale gouges taken from the full stratigraphic section at conditions typifying the reservoir depth. Velocity-stepping experiments were performed on representative shale gouges at a confining pressure of 60 MPa, pore fluid pressure of 30 MPa, and temperature of 150°C. Results show the gouges are generally frictionally strong with friction coefficients ranging between 0.50 and 0.75. Two phyllosilicate + TOC (total organic carbon)-poor gouges exhibited higher frictional strength and velocity weakening, capable of potentially unstable fault slip, while only velocity strengthening was observed for the remaining phyllosilicate + TOC-rich gouges. These results confirm that the frictional and stability properties are mainly controlled by phyllosilicate + TOC content. Elevating the temperature further weakens the gouges and drives it toward velocity weakening. The presence of observed seismicity in a majority of velocity-strengthening materials suggests the importance of the velocity-weakening materials. We suggest a model where seismicity is triggered when pore fluid pressures drive aseismic slip and triggers seismic slip on adjacent faults in the same formation and distant faults in the formations above/below. The effect of pore pressure transients within low-permeability shale gouges is incorporated. Our results highlight the importance of understanding mechanisms of induced earthquakes and characterizing fault properties prior to hydraulic fracturing. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词	aseismic slip; fault gouge; hydraulic fracturing; mineral variation; shale; strength and stability
语种	英语
来源期刊	Journal of Geophysical Research: Solid Earth
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/187691
作者单位	Department of Geotechnical Engineering, College of Civil Engineering, Tongji University, Shanghai, China; Key Laboratory of Geotechnical and Underground Engineering of Ministry of Education, Tongji University, Shanghai, China; Department of Energy and Mineral Engineering, EMS Energy Institute and G3 Center, Pennsylvania State University, University Park, PA, United States; Department of Geosciences, Pennsylvania State University, University Park, PA, United States; PetroChina Hangzhou Institute of Geology, Hangzhou, China; CNPC Engineering Technology R&D Company Limited, Beijing, China; Department of Civil and Architectural Engineering and Mechanics, University of Arizona, Tucson, AZ, United States
推荐引用方式 GB/T 7714	An M.,Zhang F.,Elsworth D.,et al. Friction of Longmaxi Shale Gouges and Implications for Seismicity During Hydraulic Fracturing[J],2020,125(8).
APA	An M.,Zhang F.,Elsworth D.,Xu Z.,Chen Z.,&Zhang L..(2020).Friction of Longmaxi Shale Gouges and Implications for Seismicity During Hydraulic Fracturing.Journal of Geophysical Research: Solid Earth,125(8).
MLA	An M.,et al."Friction of Longmaxi Shale Gouges and Implications for Seismicity During Hydraulic Fracturing".Journal of Geophysical Research: Solid Earth 125.8(2020).