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Journal of the Geological Society, 1976
The mineralogy and textures of sedimentary carbonate rocks suggest two stages of diagenesis. The stabilization of skeletal fragments from aragonite, high magnesian calcite and calcite, to calcite is the first stage and generally pre-compactive grain fracture.
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The mineralogy and textures of sedimentary carbonate rocks suggest two stages of diagenesis. The stabilization of skeletal fragments from aragonite, high magnesian calcite and calcite, to calcite is the first stage and generally pre-compactive grain fracture.
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Classifications of Carbonate Rocks
1982Carbonate rocks can be subdivided according to: a) chemical and mineralogical composition, e.g., Chilingar (1960), Pettijohn (1957), or Fuchtbauer (1959), b) fabric features — “groundmass” (= matrix and/or cement) and particles, c) special physical parameters, e.g., porosity, Choquette and Pray (1970); see 9.2.1.
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Microporosity of Carbonate Rocks
1968Consolidated carbonate rocks have relative low porosities but high specific surface areas thus showing a fine dispersion of the pore volume. The pore radii distribution derived from Hg-capillary pressure curves show maxima which are in good accordance with the grain size distribution.
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Matrix acidizing in carbonate rocks and the impact on geomechanical properties: A review
Fuel, 2023Ahmed Z Al-Yaseri
exaly