Abu Dhabi International Petroleum Conference and Exhibition 2012
DOI: 10.2118/162342-ms
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Characterisation and Modeling of Fractures in Large Onshore Abu Dhabi Carbonate Field

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Cited by 8 publications
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“…Interestingly, the NW-SE Profile 3 does not image any faults. This is because the seismic Profiles 3 and 11 (Figs 6 and 9) are parallel to the major N75˚W and N45˚W faults imaged in the Asab anticline (Sirat, 2015;Sirat et al, 2012b).…”
Section: Asab Anticlinementioning
confidence: 97%
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“…Interestingly, the NW-SE Profile 3 does not image any faults. This is because the seismic Profiles 3 and 11 (Figs 6 and 9) are parallel to the major N75˚W and N45˚W faults imaged in the Asab anticline (Sirat, 2015;Sirat et al, 2012b).…”
Section: Asab Anticlinementioning
confidence: 97%
“…However in general, fault density and throw appear to increase near fold axes, in particular in the Asab and Sahil anticlines, suggesting that folding and faulting may be coeval (Johnson et al, 2005). However, Sirat et al (2012aSirat et al ( , 2012bSirat et al ( , 2013 and Sirat (2015) suggested that the N75˚W faults are pre-folding and formed as tensile fractures when the maximum horizontal stress was oriented at 120˚ during the Early Cretaceous; whereas the N45˚W are post-folding and formed as splays from N75˚W faults when the maximum horizontal stress was oriented east-west. The northward movement of the Indian plate and obduction of the Masirah Ophiolite during the Maastrichtian -Paleocene is inferred to have caused counter-clockwise rotation of the maximum horizontal stress axis, which resulted in the development of the N75˚W faults (Sirat, 2015).…”
Section: Timing and Growth Of Faulting And Foldingmentioning
confidence: 97%