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Journal of Petroleum Technology, 2010
This article, written by Senior Technology Editor Dennis Denney, contains highlights of paper IPTC 13850, ’Carbonate-Rock Physics Issues,’ by Enru Liu, Michael A.Payne, Shiyu Xu, Gregor Baechle, and Christopher E. Harris, ExxonMobil Upstream Research, prepared for the 2009 International Petroleum Technology Conference, Doha, Qatar, 7-9 December.
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This article, written by Senior Technology Editor Dennis Denney, contains highlights of paper IPTC 13850, ’Carbonate-Rock Physics Issues,’ by Enru Liu, Michael A.Payne, Shiyu Xu, Gregor Baechle, and Christopher E. Harris, ExxonMobil Upstream Research, prepared for the 2009 International Petroleum Technology Conference, Doha, Qatar, 7-9 December.
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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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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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Wettability alteration of locally synthesized cationic gemini surfactants on carbonate rock
Journal of Molecular Liquids, 2021Muhammad Shahzad Kamal, Shirish Patil
exaly

