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- W2183638229 abstract "Fe-chlorite bearing sandstones are present in many basins of different age; owi ng to the presence of por e-lining/pore-filling F e (and Mg)-chlorite they are a reservoir even in high depth/high temperature regimes. On th e other side, the abundance and thickness o f the coatings is a limiting factor for permeability; in order to pred ict the reservoir qualit y, it is thus important to understand the factors that influence the chlorite coatings growth. As the chlorite-bearing reservoirs are depos ited in specific settings, and namely in the transitional environments, where mixin g between Fe-rich fresh waters and marine wate rs occurs, it is mandatory to sort out th e effect of textural parameters (grain-size and sorting) and of grain composition on chlor ite abundance. The grain composition is also affecting the type (Mg vs. Fe-Chlorite) and crystalline structure (platelets vs. filaments) of the chlorite that will form on grain surfaces." @default.
- W2183638229 created "2016-06-24" @default.
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- W2183638229 date "2009-01-01" @default.
- W2183638229 modified "2023-09-27" @default.
- W2183638229 title "The Chlorite-Bearing Reservoirs: E ffects of the Main Petrographic Para meters on Reservoir Quality*" @default.
- W2183638229 hasPublicationYear "2009" @default.
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