Finite element modelling of Gassmann fluid substitution of heterogeneous rocks
The traditional method of fluid substitution requires the rock to be microhomogeneous with a fully connected porespace that ensures hydraulic equilibrium of the pore fluid. These assumptions may be violated for multimineral rocks, such as shaley sediments, due to a large contrast in elastic properti...
| Main Authors: | , , |
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| Other Authors: | |
| Format: | Conference Paper |
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Co-productions
2007
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| Online Access: | http://hdl.handle.net/20.500.11937/18989 |