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Volume change during sediment diagenesis and the development of growth faults
Authors:Mervyn E Jones  Michael A Addis
Institution:Department of Geology, Kings College London, Strand, London WC 2, UK
Abstract:The stress system induced the weight of a sediment and the pore fluid it contains, termed the passive stress system, is capable of deforming the sediment. This volumetric deformation is examined with respect to the evolution of porosity and permeability during burial. The effect of this self deformation on the shape of growth faults and normal faults in extensional terrains is considered.
Keywords:Consolidation  Effective stress  Growth fault  Listric fault  Overpressured pore fluids  Permeability  Porosity  Stress path
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