Poroelastic responses of confined aquifers to subsurface strain and their use for volcano monitoring
Well water level changes associated with magmatic unrest can be interpreted as a result of pore pressure changes in the aquifer due to crustal deformation, and so could provide constraints on the subsurface processes causing this strain. We use finite element analysis to demonstrate the response of...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2015-11-01
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| Series: | Solid Earth |
| Online Access: | http://www.solid-earth.net/6/1207/2015/se-6-1207-2015.pdf |