Abstract:The last marine cycle of Dubai Lower-Cretaceous has left reefal carbonate deposits on paleo-highs from deep basement faults. Those shores face deposits at the edge of the former Bab basin and developed very good reservoir but had a prolonged emersion prior to the deposition of Nahr Umr seal and are often karstified. A successful development relied on high-angle drilling through an unstable seal and advance geosteering within a complex reservoir with a thin oil leg.
A unique drilling approach in … Show more
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