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Strength recovery of solid contacts under fluid flow conditions

Strength recovery of solid contacts under fluid flow conditions
流体流动条件下固体接触的强度恢复
批准号:
19K21907
负责人:
HIROSE Takehiro
金额:
$3.91万
依托单位国家:
日本
项目类别:
Grant-in-Aid for Challenging Research (Exploratory)
财政年份:
2019
资助国家:
日本
项目状态:
已结题
起止时间:
2019-06-28 至 2023-03-31

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期刊论文(30)
专著(0)
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会议论文
DOI: 10.1016/j.gca.2019.04.010
发表时间: 2019-06
期刊: Geochimica et Cosmochimica Acta
影响因子: 5
作者: [Paul A. Wallace;Sarah H. De Angelis;A. Hornby;J. Kendrick;S. Clesham;Felix W. von Aulock;Amy Hughes;J. Utley;T. Hirose;Donald Bruce Dingwell;Y. Lavallée]
通讯作者: Paul A. Wallace;Sarah H. De Angelis;A. Hornby;J. Kendrick;S. Clesham;Felix W. von Aulock;Amy Hughes;J. Utley;T. Hirose;Donald Bruce Dingwell;Y. Lavallée
Formation of clast-cortex aggregates in experimental fault gouges
实验断层泥中碎屑皮层聚集体的形成
DOI: 10.1016/j.tecto.2022.229524
发表时间: 2022
期刊: Tectonophysics
影响因子: 2.9
作者: [Kim Jae Hoon, Ree Jin-Han, Hirose Takehiro, Oohashi Kiyokazu]
通讯作者: Oohashi Kiyokazu
Frictional stability of porous tuff breccia under subsurface pressure conditions and implications for shallow seismicity
地下压力条件下多孔凝灰岩角砾岩的摩擦稳定性及其对浅层地震活动的影响
DOI: 10.1186/s40623-021-01419-y
发表时间: 2021
期刊: Earth, Planets and Space
影响因子: --
作者: [Mizoguchi Kazuo, Uehara Shin-ichi, Hirose Takehiro, Iizuka Sachiko]
通讯作者: Iizuka Sachiko
Weakening of quartz rocks at subseismic slip rates due to frictional heating, but not to lubrication by wear materials of hydrated amorphous silica or silica gel
由于摩擦加热,石英岩在次震滑移率下被削弱,但不是由于水合无定形二氧化硅或硅胶磨损材料的润滑
DOI: 10.1016/j.tecto.2020.228429
发表时间: 2020
期刊: Tectonophysics
影响因子: 2.9
作者: [Kanagawa, K., Murayama, H., Sugita, A., Takahashi, M., Sawai, M., Furukawa, N. and Hirose, T.]
通讯作者: T.
28
    Earthquakes as a potential energy source for subsurface deep biosphere
    Physicochemical mechanisms underlying frictional responses at slow to fast earthquakes: inferred from hydrothermal friction experiments
    Asperity of seismogenic faults from geological point of view
    Hydrogen generation by earthquake faulting and its implication for sub-surface biosphere
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