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Morency, Christina - Department of Geosciences, Princeton University
Computational poroelasticity --A review Jos M. Carcione1
568 The Leading Edge May 2009 SPECIAL SECTION: S e i s m i c m o d e l i n gS e i s m i c m o d e l i n g
A numerical model for coupled fluid flow and matrix deformation with applications to disequilibrium compaction
4D seismic monitoring of CO2 sequestration based upon spectral-element and adjoint methods: com-parison of acoustic, elastic and poroelastic theories
Geophys. J. Int. (2008) 175, 301345 doi: 10.1111/j.1365-246X.2008.03907.x GJISeismology
Spectral-Element Simulations of Wave Propagation in Porous Media: Finite-Frequency Sensitivity Kernels
Elastic imaging and time-lapse migration based on adjoint methods , Yang Luo1
Geophys. J. Int. (2009) doi: 10.1111/j.1365-246X.2009.04332.x GJISeismology
Continental rifting as a function of lithosphere mantle strength Frdric Gueydan , Christina Morency 1
Three-dimensional numerical simulations of mantle flow beneath mid-ocean ridges
Numerical simulations of the mantle lithosphere delamination C. Morency and M.-P. Doin
Convective destabilization of a thickened continental lithosphere