Fracture porosity. Porosity and permeability follow tectonic geometry and mechanical stratigraphy, not depositional or diagenetic boundaries (Stearns and Friedman, 1972; Corbett et al., 1991).

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Fracture porosity. Porosity and permeability follow tectonic geometry and mechanical stratigraphy, not depositional or diagenetic boundaries (Stearns and Friedman, 1972; Corbett et al., 1991).