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Sequence stratigraphy of carbonate rocks
The Leading Edge, 1999In the first contribution to TLE’s Geologic Column, J. M. Mulholland concluded that “sequence stratigraphy … is a tool that every explorationist must master.” I agree. In fact, sequence stratigraphy is more than a versatile tool in exploration and production geology. It is in many ways a role model for applied earth sciences.
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Stylolitization in Carbonate Rocks
1968Stylolite features are defined in terms of rock grain fabric relationships: intergranular and aggregate stylolites are differentiated. Geometric and genetic classifications of stylolites are offered. Megascopic and microscopic observations on the stylolites occuring in carbonate rocks of the Uppper Mississippian System in southern Illinois fluorspar ...
Won-choon Park, Erik H. Schot
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1980
Abstract This core workshop is the product of an effort by the SEPM Carbonate Research Group to emphasize the value of careful core interpretation to hydrocarbon exploration and production programs. Initially conceived as a small conference the format was expanded in response to strong interest from the geologic community.
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Abstract This core workshop is the product of an effort by the SEPM Carbonate Research Group to emphasize the value of careful core interpretation to hydrocarbon exploration and production programs. Initially conceived as a small conference the format was expanded in response to strong interest from the geologic community.
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Stochastic multiscale model for carbonate rocks
Physical Review E, 2007A multiscale model for the diagenesis of carbonate rocks is proposed. It captures important pore scale characteristics of carbonate rocks: wide range of length scales in the pore diameters; large variability in the permeability; and strong dependence of the geometrical and transport parameters on the resolution.
B, Biswal +4 more
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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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1994
Abstract The main factors in evaluating carbonate reservoirs are lithofacies, pore types, shelf setting, sequence stratigraphy, and diagenetic overprint. Several patterns are evident based on a review of carbonate reservoirs from around the world.
Clifton F. Jordan, James Lee Wilson
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Abstract The main factors in evaluating carbonate reservoirs are lithofacies, pore types, shelf setting, sequence stratigraphy, and diagenetic overprint. Several patterns are evident based on a review of carbonate reservoirs from around the world.
Clifton F. Jordan, James Lee Wilson
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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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Environmental Earth Sciences, 2016
Carbon dioxide (CO2) storage in aquifers or injection to petroleum reservoirs for enhanced oil recovery purposes are the ways of mitigation of global warming. Dissolution of carbon dioxide in water forms carbonic acid. This acid would react with the carbonate components in carbonate rocks (i.e., CaCO3, MgCO3) and cause dissolution of salts thereafter ...
Mohsen Abbaszadeh +2 more
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Carbon dioxide (CO2) storage in aquifers or injection to petroleum reservoirs for enhanced oil recovery purposes are the ways of mitigation of global warming. Dissolution of carbon dioxide in water forms carbonic acid. This acid would react with the carbonate components in carbonate rocks (i.e., CaCO3, MgCO3) and cause dissolution of salts thereafter ...
Mohsen Abbaszadeh +2 more
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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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