2010
DOI: 10.1016/j.marpetgeo.2009.12.002
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Pore system characterisation in heterogeneous carbonates: An alternative approach to widely-used rock-typing methodologies

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Cited by 158 publications
(96 citation statements)
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References 25 publications
(23 reference statements)
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“…According to (10), water saturation, porosity, permeability, and oil column height relationship can be obtained by multiple regressions. The oil column height can be calculated based on the depth difference between water/oil contact and grid depth, and the water saturation is calculated for each grid.…”
Section: D Water Saturation Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…According to (10), water saturation, porosity, permeability, and oil column height relationship can be obtained by multiple regressions. The oil column height can be calculated based on the depth difference between water/oil contact and grid depth, and the water saturation is calculated for each grid.…”
Section: D Water Saturation Modelmentioning
confidence: 99%
“…Rock typing is an essential step in the process of the carbonate reservoir characterization and geological modeling, and it is the method of classifying reservoir rocks which have the same fluid flow features into groups [1][2][3][4][5][6]. Rock typing is an effective way to obtain accurate permeability, and it enables us to get better understanding of the fluid movement and to enhance oil recovery [7][8][9][10][11].…”
Section: Introductionmentioning
confidence: 99%
“…Cement precipitation (drusy or blocky) and/or by matrix during deposition or post-deposition by compaction processes can clog the pores resulting in lower permeability (Tucker, 2009;Lucia, 2007). Drusy calcite cement is thought to be a sign of early diagenesis in a meteoric environment, whereas the saddle dolomite and the fluorite mineral are believed to be formed by circulation of hydrothermal fluids at a deep (Flügel, 2004;Tucker, 2009;Lambert et al, 2006;Hollis et al, 2010;Alsharhan and Nairn, 1990). It is also believed to have occurred after reaching burial depth of around 600 m at temperatures of around 65.6°C (Cox et al, 2010).…”
Section: Cementationmentioning
confidence: 99%
“…However, ignoring the geological controls such as pore space evolution is caused by the focus on grouping samples with consistent petrophysical properties, rather than geological characteristics. It is also problematic to achieve a fit-for-purpose rock-typing scheme separate from the influence of diagenetic processes on characteristics such as rock petrophysic, hydrocarbon recovery efficiency and fluid in-place volumes [1] [2] [3] [4] and [5]. Integrating large scale dynamic data to the wireline scale (small scale) is another inevitable challenge.…”
Section: Introductionmentioning
confidence: 99%