Seismicity-permeability coupling in the behavior of gas shales, CO2 storage and deep geothermal energy

Author:

Fang Y.,Wang C.,Elsworth D.,Ishibashi T.

Publisher

Springer Science and Business Media LLC

Subject

Economic Geology,General Energy,Geophysics,Geotechnical Engineering and Engineering Geology

Reference52 articles.

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2. Abe S, Mair K (2009) Effects of gouge fragment shape on fault friction: new 3D modelling results. Geophys Res Lett 36(23):2–5. doi: 10.1029/2009GL040684

3. Allis R, Chidsey T, Gwynn W, Morgan C, White S, Adams M, Moore J (2001) Natural CO2 reservoirs on the Colorado Plateau and southern Rocky Mountains: candidates for CO2 sequestration. In: Proceedings of the first national conference on carbon sequestration. pp 14–17

4. Anderson RN, Zoback MD (1982) Permeability, underpressures, and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial Pacific. J Geophys Res 87(B4):2860. doi: 10.1029/JB087iB04p02860

5. Anderson JG, Wesnousky SG, Stirling MW (1996) Earthquake size as a function of fault slip rate. Bull Seismol Soc Am 86(3):683–690

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