| DOI: | 10.1016/j.epsl.2020.116682
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| 论文题名: | Velocity-weakening friction induced by laboratory-controlled lithification |
| 作者: | Ikari M.J.; Hüpers A.
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| 刊名: | Earth and Planetary Science Letters
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| ISSN: | 0012821X
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| 出版年: | 2021
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| 卷: | 554 | | 语种: | 英语
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| 中文关键词: | cohesion
; diagenesis
; fault
; friction
; lithification
; seismogenic zone
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| 英文关键词: | Chloride minerals
; Earthquakes
; Faulting
; Friction
; Porosity
; Powders
; Shale
; Sodium chloride
; Direct measurement
; Earthquake nucleation
; Friction parameters
; Frictional behavior
; Frictional properties
; Microstructural images
; Unconsolidated sediment
; Velocity-weakening
; Velocity
; cementation
; diagenesis
; fault zone
; halite
; instability
; lithification
; porosity
; seismicity
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| 英文摘要: | Regarding the occurrence of seismicity on major plate-boundary fault zones, one leading hypothesis is that the processes of lithification is responsible transforming loose, unconsolidated sediment that does not host earthquake nucleation into the frictionally unstable rocks that inhabit the seismogenic zone. Previous laboratory studies comparing the frictional properties of intact rocks and powdered versions of the same rocks generally support this hypothesis. However, systematically quantifying frictional behavior as a function of lithification remains a challenge. Here, we simulate the lithification process in the laboratory by consolidating mixtures of halite and shale powders with halite-saturated brine, which we then desiccate. The desiccation allows precipitation of halite as cement, creating synthetic rocks. We quantify lithification by: (1) direct measurement of cohesion, and (2) measuring the porosity reduction of lithified samples compared to powders. We observe that powdered samples of each halite-shale proportion exhibit predominantly velocity-strengthening friction, whereas lithified samples exhibit a combination of velocity strengthening and significant velocity weakening when halite constitutes at least 30 wt% of the sample. Analysis of the individual rate-dependent friction parameters shows that the occurrence of velocity weakening is due to relatively low values of a for lithified samples. Larger velocity weakening is associated with cohesion of >∼1 MPa, and porosity reduction of >∼50 vol%. Microstructural images reveal that the shear surfaces for powders tend to exhibit small cracks not seen on the lithified sample shear surfaces. Our results suggest that lithification via cementation and porosity loss can facilitate slip instability, supporting the lithification hypothesis for seismogenic slip. © 2020 The Authors |
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| 资源类型: | 期刊论文
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| 标识符: | http://119.78.100.158/handle/2HF3EXSE/165521
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| Appears in Collections: | 气候变化与战略
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作者单位: | MARUM Center for Marine Environmental Sciences, Faculty of Geosciences, University of Bremen, Germany
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| Recommended Citation: | |
Ikari M.J.,Hüpers A.. Velocity-weakening friction induced by laboratory-controlled lithification[J]. Earth and Planetary Science Letters,2021-01-01,554
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