All Days 2010
DOI: 10.2118/137663-ms
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Developed Approach for Better Understanding of Low Resistivity Pay Carbonate Reservoirs

Abstract: Some of the Middle East UAE lower Cretaceous Thamama Carbonate reservoirs are characterized by low resistivity pay phenomena, on which log analysis results in high water saturation computation; on the contrary, production tests confirm dry oil. The Sedmintological investigation on thin sections have shown significant percentage of Micro-porous (occluded porosity or non-efficient porosity) network traps irreducible hyper-saline formation water which responds to a low resistivity, even if the oil … Show more

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Cited by 8 publications
(5 citation statements)
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“…Additionally, the LRP intervals are commonly identified with high water saturation, which makes such intervals of low interest to the extent that they are discarded as attractive to appraise, particularly when oil prices are low. Typically, LRP zones are characterized by formation interval, with moderate to high porosities, showing extremely low resistivity that are often less than 3 X-m and most frequently encountered in areas with saline formation water (Griffiths et al 2006;Obeidi et al 2010;Worthington 2000;Farouk et al 2014;Uchida et al 2015). While Boyd et al (1995) proposed that the resistivity range is between 0.5 and 5 X-m, several other researchers, like Zhao et al (2000), stated that LRP can be identified by the ratio of the pay zone to the water-bearing zone and this ratio is considered to be in the range of 2.…”
Section: Introductionmentioning
confidence: 99%
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“…Additionally, the LRP intervals are commonly identified with high water saturation, which makes such intervals of low interest to the extent that they are discarded as attractive to appraise, particularly when oil prices are low. Typically, LRP zones are characterized by formation interval, with moderate to high porosities, showing extremely low resistivity that are often less than 3 X-m and most frequently encountered in areas with saline formation water (Griffiths et al 2006;Obeidi et al 2010;Worthington 2000;Farouk et al 2014;Uchida et al 2015). While Boyd et al (1995) proposed that the resistivity range is between 0.5 and 5 X-m, several other researchers, like Zhao et al (2000), stated that LRP can be identified by the ratio of the pay zone to the water-bearing zone and this ratio is considered to be in the range of 2.…”
Section: Introductionmentioning
confidence: 99%
“…While Boyd et al (1995) proposed that the resistivity range is between 0.5 and 5 X-m, several other researchers, like Zhao et al (2000), stated that LRP can be identified by the ratio of the pay zone to the water-bearing zone and this ratio is considered to be in the range of 2. LRP occurs in both clastics and carbonates, while in carbonates, it has been reported to be as a result of either or a combination of deep high saline mud invasion, presence of conductive minerals, presence of microporosity, and anisotropic effect due to drilling high angle wells within thin reservoirs (Griffiths et al 2006;Obeidi et al 2010;Chu and Steckhan 2011). Most especially, tight carbonates are often affected by the deep invasion of conductive mud filtrate, which consecutively affects deep resistivity reading (Souvick 2003).…”
Section: Introductionmentioning
confidence: 99%
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“…LRPZs take place and have reported from both clastic and carbonate reservoirs, in carbonates. It has been reported to be as a result of either or a combination of deep high saline mud invasion, presence of conductive minerals, presence of microporosity, and anisotropic effect due to drilling high angle wells within reservoirs [4] [5]. Typically, LRP zones are characterized by formation interval, with moderate to high porosities, showing extremely low resistivity less than 1 ohm meter.…”
Section: Introductionmentioning
confidence: 99%
“…Such micropores can be present within highly micritized skeletal grains (micritic envelopes surrounding fossils and microbial dominated fossils) as well as non-skeletal grains (ooids and peloids). The trapped water within micropores is often highly saline, as high as 200,000 ppm of NaCl (Obiedi et al 2010). The micropores often form an interconnected network containing formation water that provides a continuous path for the measured electric current resulting in a low resistivity reading, and causing a significant underestimation of the true oil saturation.…”
Section: Introductionmentioning
confidence: 99%