A quantitative comparison of some mechanisms generating overpressure in sedimentary basins
- 15 June 2001
- journal article
- Published by Elsevier BV in Tectonophysics
- Vol. 334 (3-4), 211-234
- https://doi.org/10.1016/s0040-1951(01)00064-6
Abstract
No abstract availableKeywords
This publication has 28 references indexed in Scilit:
- Temperature-dependent viscoelastic compaction and compartmentalization in sedimentary basinsTectonophysics, 2000
- Compaction-driven fluid flow in viscoelastic rockGeodinamica Acta, 1998
- Effects of burial diagenesis on stresses, compaction and fluid flow in sedimentary basinsMarine and Petroleum Geology, 1997
- Compaction and overpressuring in Pleistocene sediments on the Louisiana Shelf, Gulf of MexicoMarine and Petroleum Geology, 1996
- Mathematical modelling of gravitational compaction and clay dehydration in thick sediment layersGeophysical Journal International, 1995
- A unified approach to geopressuring, low‐permeability zone formation, and secondary porosity generation in sedimentary basinsJournal of Geophysical Research, 1994
- Effective stress for transport properties of inhomogeneous porous rockJournal of Geophysical Research, 1992
- A mathematical model for compaction in sedimentary basinsGeophysical Journal International, 1992
- Linear and nonlinear solutions for one‐dimensional compaction flow in sedimentary basinsWater Resources Research, 1988
- On the Maintenance of Anomalous Fluid Pressures: I. Thick Sedimentary SequencesGSA Bulletin, 1968