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Title: Depositional environment, reservoir units evolution, and hydrocarbon habitat of Shuaiba formation, Lower Cretaceous, Abu Dhabi, United Arab Emirates

Journal Article · · Am. Assoc. Pet. Geol., Bull.; (United States)
OSTI ID:5172674

The Shuaiba Formation (Aptian) is a thick, porous shelf carbonate, present in the subsurface over much of the Arabian Gulf. It is the uppermost formation of the Thamama Group (Lower Cretaceous), and is overlain by the Nahr Umr Formation (Albian) and overlies the Kharaib Formation (Barremian). The formation is divided into nine reservoir units. The major reefal Shuaiba buildup in Abu Dhabi trends northwest-southeast. It is in this trend that the major oil fields (Shah, Bu Hasa, and Zurarah-Shaybah) were discovered and from which some wells produce in western Abu Dhabi (e.g., Ruwais-2). Hydrocarbons also occur outside of the rudist trend in the Shuaiba Formation in the Asab, Jarn Yaphour, and Sahil onshore oil fields, and the Zakum and Mandous offshore oil fields. Geochemical studies reveal that the main source for the Thamama oils are the Upper Jurassic Dukhan Formation (onshore Abu Dhabi) or Diyab Formation (offshore Abu Dhabi), however, some Shuaiba source rocks may have existed in intrashelf basinal areas in the upper Thamama zone. The Nahr Umr Shale acts as a seal for the Shuaiba reservoir in this area.

Research Organization:
Department of Geology, University of South Carolina, Columbia, South Carolina
OSTI ID:
5172674
Journal Information:
Am. Assoc. Pet. Geol., Bull.; (United States), Vol. 69:6
Country of Publication:
United States
Language:
English