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The frictional sliding properties of antigorite gouge under hydrothermal conditions
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Shimin Liua, b, Mengke Anc, Wenhao Daib, d, *, Huiru Leib, Lei Zhangb, Yongsheng Zhoub, Zekang Yangb
Rock Mechanics Bulletin | 2026, 5(2) : 100244
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Rock Mechanics Bulletin | 2026, 5(2): 100244
The frictional sliding properties of antigorite gouge under hydrothermal conditions
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Shimin Liua, b, Mengke Anc, Wenhao Daib, d, *, Huiru Leib, Lei Zhangb, Yongsheng Zhoub, Zekang Yangb
Affiliations
  • aSchool of Fire Protection Engineering, China People's Police University, Langfang, 065000, China
  • bState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake Administration, Beijing, 100029, China
  • cDepartment of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, 100872, China
  • dJiangxi Earthquake Agency, Nanchang, 330026, China
Published: 2026-04-10 doi: 10.1016/j.rockmb.2025.100244
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As a weak mineral overlying subduction-zone faults, the widespread presence of antigorite can markedly affect subduction-zone dynamics. To better understand the mechanical properties of antigorite-bearing faults, we conducted frictional sliding experiments on antigorite under hydrothermal conditions. The experimental setup involved a constant confining pressure of 100 MPa, a low pore fluid pressure of 30 MPa, and temperatures ranging from 100 ℃ to 500 ℃. We varied the axial loading rate between 0.04, 0.2, and 1.0 μm/s to examine the velocity dependence of the friction coefficient. The results showed that the friction coefficient of antigorite exhibited a significant temperature dependence. Between 100 ℃ and 400 ℃, the friction coefficient decreased from 0.66 to 0.54 as the temperature increased. Above 400 ℃, the friction coefficient increased, reaching 0.7. The velocity dependence of antigorite exhibited velocity strengthening (a - b > 0) throughout the entire experimental temperature range (100 ℃-500 ℃). The impact of pore-fluid pressure on the frictional behavior of antigorite was also significant. Under low pore-fluid pressure (30 MPa), the frictional strength increases above 400 ℃, associated with dehydration hardening. In contrast, at high pore fluid pressure, frictional weakening continues at elevated temperatures, indicating that pore fluid pressure plays a crucial role in regulating the frictional stability of antigorite. Our experimental results demonstrate that the pore fluid pressure plays a key role in regulating the temperature-dependent frictional behavior of antigorite, highlighting the need for further investigation under varying fluid pressure conditions.

Antigorite  /  Friction coefficient  /  Velocity dependence  /  Steady sliding  /  Pore fluid pressure
Shimin Liu, Mengke An, Wenhao Dai, Huiru Lei, Lei Zhang, Yongsheng Zhou, Zekang Yang. The frictional sliding properties of antigorite gouge under hydrothermal conditions[J]. Rock Mechanics Bulletin, 2026 , 5 (2) : 100244 - . DOI: 10.1016/j.rockmb.2025.100244
  • Langfang Science and Technology Research and Development Program(2024013158)
  • Langfang Science and Technology Bureau and the National Natural Science Foundation of China(42494862)
Year 2026 volume 5 Issue 2
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Article Info
doi: 10.1016/j.rockmb.2025.100244
  • Receive Date:2025-06-13
  • Online Date:2026-06-17
  • Published:2026-04-10
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History
  • Received:2025-06-13
  • Revised:2025-07-23
  • Accepted:2025-08-29
Funding
Langfang Science and Technology Research and Development Program(2024013158)
Langfang Science and Technology Bureau and the National Natural Science Foundation of China(42494862)
Affiliations
    aSchool of Fire Protection Engineering, China People's Police University, Langfang, 065000, China
    bState Key Laboratory of Earthquake Dynamics and Forecasting, Institute of Geology, China Earthquake Administration, Beijing, 100029, China
    cDepartment of Civil and Environmental Engineering, The Hong Kong Polytechnic University, Hong Kong, 100872, China
    dJiangxi Earthquake Agency, Nanchang, 330026, China

Corresponding:

* Corresponding author. E-mail address: (W. Dai).
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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