Interaction between deformation sources and implications for numerical modelling of magma storage
Volcano ground deformation due to magma movement in the subsurface is commonly modelled using simple point (Mogi) or dislocation (Okada) sources, embedded in a homogeneous, isotropic, elastic half-space, and representing respectively a magma chamber and a dike. When datasets are too complex to be ex...
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University of Leeds
2013
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.595131 |