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Abstract

The east of the Emirate of Dubai is dominated by the geologically complex western thrust front of the<br>northern Omani Mountains. This deformation front is the boundary between the western foredeep basin<br>and the eastern Omani fold-and-thrust belt.<br>Complex geology makes conventional exploration challenging. The reservoir (Thamama Group)<br>structures are thrusted anticlines with the overlying Tertiary units showing large-scale thrusting as well.<br>The Lower Cretaceous Thamama Group limestone is one of the main hydrocarbon reservoirs in the<br>Middle East. It forms a major hydrocarbon-producing reservoir in the U.A.E., Iraq, Bahrain and Oman<br>and has a high hydrocarbon potential in southeast Iraq, offshore Oman and offshore northeast Saudi Arabia.

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/content/papers/10.3997/2214-4609-pdb.248.087
2010-03-07
2024-04-27
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