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Abstract

The Upper Jurassic Arab-C Reservoir in the Dukhan Field is the product of a stable epicontinental shelf subjected to continuous relative sea-level variations, with the preserved sediments representing a complex of syndepositional carbonate lithologies and textures deposited in subtidal, intertidal and sabkha environments. Though the depositional units are spatially correlated within a sequencestratigraphic context, petrophysical observations do not conform to the primary depositional fabric, and a cross-cutting relationship is observed.

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/content/papers/10.3997/2214-4609.20142794
2012-12-09
2024-04-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20142794
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