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The definition of hydraulic properties of fault zones is a major issue in structural geology, seismology, and in several applications (hydrocarbons, hydrogeology, CO2 sequestration, etc.). The permeability of fault rocks can be measured in laboratory
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4e4bc922fbedc92f608afb80868172a2
http://hdl.handle.net/11585/261297
http://hdl.handle.net/11585/261297
Autor:
Mittempergher, Silvia, DI TORO, Giulio, Gratier JP, 2, Hadizadeh, J, Smith, Saf, Spiess, Richard
Publikováno v:
Geophysical Research Letters
Geophysical Research Letters, American Geophysical Union, 2011, 38, pp.L03301. ⟨10.1029/2010GL046129⟩
Geophysical Research Letters, 2011, 38, pp.L03301. ⟨10.1029/2010GL046129⟩
Geophysical Research Letters, American Geophysical Union, 2011, 38, pp.L03301. ⟨10.1029/2010GL046129⟩
Geophysical Research Letters, 2011, 38, pp.L03301. ⟨10.1029/2010GL046129⟩
6p.; International audience; The San Andreas Fault Observatory at Depth (SAFOD) in Parkfield, central California, has been drilled through a fault segment that is actively deforming through creep and microearthquakes. Creeping is accommodated in two
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ce1931ef656b29ba515b51d5567ed699
https://hal-insu.archives-ouvertes.fr/insu-00681315/file/2010GL046129.pdf
https://hal-insu.archives-ouvertes.fr/insu-00681315/file/2010GL046129.pdf