Compaction-Induced Permeability Loss’s Effect on Induced Seismicity During Reservoir Depletion
Producing fluid out of subsurface reservoirs causes stress changes that can lead to induced seismicity. In the fully coupled theory of poroelasticity, these stress changes are caused by the gradient of pore pressure which acts as an internal force in the momentum balance equation. This implies that,...
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Published in | Pure and applied geophysics Vol. 176; no. 10; pp. 4277 - 4296 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Cham
Springer International Publishing
01.10.2019
Springer Nature B.V Springer Verlag |
Subjects | |
Online Access | Get full text |
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