作者: M Person , L.B Goodwin , G Rawlings , S Connell
DOI: 10.1016/S0375-6742(00)00061-3
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摘要: Abstract We propose a new model to represent the spatial and temporal evolution of fault permeability within poorly lithified sediments. The utilizes an advection–dispersion equation transport mixing sand clay size material, which become entrained into zone. is being tested using mathematical modeling constrained by sedimentological permeability, cementation data collected along Sand Hill Fault Albuquerque Basin Rio Grande Rift.