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Middle East Models Conference Abstracts Jurrasic/Cretaceous Jurassic/Cretaceous Carbonate Platform - Basin Systems: Middle East Models Conference Abstracts precipitation of neomorphic calcite microspar in Reservoir Characterization of interparticle pore spaces within peloidal lithofacies led the Shu’aiba Formation, to the reduction of matrix microporosity and permeability Ghaba North Field, Oman and thus reservoir quality of the lower zone. Therefore, the observed spatial and vertical variability of the Abdulrahman A. Al-Awar, reservoir, in addition to fracture distribution and Dubai Petroleum Company, UAE orientation, should be considered in any infill drilling and John D. Humphrey, or flooding programs planned for the Shu’aiba. Colorado School of Mines, USA The Aptian Shu’aiba Formation is subdivided into two Sedimentologic and Palaeogeographic major reservoir zones in Ghaba North field, the lower Evolution of Syria during the and upper Shu’aiba. The lower zone was deposited in Jurassic and Cretaceous shallow inner-shelf setting with restricted to partially restricted water circulation conditions. The upper zone (Northwestern Arabian Platform) was deposited under open conditions in a shallow outer- shelf setting. The succession of facies in the Shu’aiba A. Khaled Al-Maleh indicates an overall major shallowing upward cycle University of Damascus and General Establishment of superimposed on it several meter-scale high frequency Geology and Mineral Resources, Syria cycles. and M. Mouty University of Damascus, Syria The Shu’aiba in the study area is a very heterogeneous The Syrian Jurassic and Cretaceous terranes were studied reservoir. It produces from secondary macroporosity, in detail in the mountain ranges of Palmyrides, Anti- fracture porosity, and matrix microporosity. Reservoir Labanon, Harmoum, Coastal and Kurd-Dagh. These storage capacity is controlled primarily by matrix were compared with their subsurface extensions in drill microporosity, which occurs as intercrystalline porosity holes. The structure and composition of these terranes within a microrhombic calcite matrix. Reservoir quality is dominantly carbonates with some limited clastic is enhanced vertically in proximity of two-recognized intercalations which are locally ferruginous with some subaerial exposure surfaces and laterally toward the volcanic intrusions of basaltic rocks. northeast. The lateral improvement in reservoir properties toward the northeast reflects the complexity The Jurassic and Cretaceous stratigraphic column was of the facies mosaic in the Shu’aiba depositional divided into formations, members and sequences. The environment. Sedimentologic evidence indicates that study of their characteristics and evolution provides the higher energy conditions resulted in deposition of general framework for the sedimentologic and grainier lithofacies with higher primary porosity in that palaeogeographic evolution of this important and direction. distinctive part of the Arabian Platform. Meteoric water diagenesis of the Shu’aiba led to The lithostratigraphic studies reveal that the Jurassic stabilization of the Shu’aiba matrix development of both carbonates of Syria and the adjacent areas are dominated secondary macroporosity and microporosity within by shallow-water dolostone, limestone and limited marly microrhombic calcite matrix. The regional unconformity interrelations. Beginning in the Jurassic, these strata were at the top of the Shu’aiba and the local subaerial exposure deposited in a shallow sea, transgressed the entire region surface capping a rudist bioherm within the Shu’aiba with the exception of the northeast-southwest, elongated have provided the means for this alteration. This Al Hammad Uplift in the east and southeast Syria. interpretation is supported by the decrease in secondary macroporosity and matrix permeability downward from The correlation of the geologic sections shows that since the exposure surfaces. In addition, the meteoric origin the end of the Early Jurassic, this uplift has further for the microrhombic calcite matrix is evident from the expanded. At the end of the Middle Jurassic the sea isotopic data regressed northwestward, where an important subsiding structure oriented north northeast-south southeast The upper zone in the Shu’aiba is characterized by (Homs-Lebanon trough), received in excess of 1,000 overall higher porosity and permeability values than the meters of Jurassic sediments. lower zone. This is due to proximity to exposure surfaces and to the better primary reservoir properties of the By the end of the Late Jurassic the sea regressed further lithofacies forming the high frequency cycles interpreted from the last submerged areas. Consequently, all of Syria within the outer-shelf setting. Furthermore, the remained emergent until the Cretaceous transgression development of crystal mosaic texture in the matrix of Barremian-Aptian time. instead of blocky-crystal framework texture and/or 476 Downloaded from http://pubs.geoscienceworld.org/geoarabia/article-pdf/2/4/476/4552235/meabst.pdf by guest on 30 September 2021 Jurassic/Cretaceous Carbonate Platform - Basin Systems: Middle East Models Conference Abstracts The Cretaceous sequences consist of three sedimentary The Simsima Formation in the subsurface exhibits rapid series of different facies. They are generally detrital at lateral lithologic changes both locally and regionally and the base (pre-Aptian to Aptian), neritic carbonates in the can be divided into two members which were deposited middle (Albian-Turonian), marly and pelagic limestone in two large-scale depositional cycles. The Lower in the upper part (Coniacian-Maastrichtian), with some Member is characterized by a coarsening-upward cycle phosphatic deposits locally in the upper part (Upper of lime mudstone/wackestones and rudistid packstones/ Campanian-Maastrichtian). grainstones with microcrystalline dolomites and a common fauna such as Lepidorbitoides, Orbitoides Major sedimentological cycles comprise the neritic media, Orbitoides tissoti, Loftusia as well as algae and carbonates of the Jurassic, and Cretaceous platform. echinoid debris deposited in a shallow marine setting Many stages of maximum flooding differ in appearance with occasional influxes of open marine water under according to the region. Maximum flooding is dated as moderate energy conditions. The Upper Member consists Lias, Bathonian, Callovian and Oxfordian- of black, argillaceous/organic matter, rudistid and bio- Kimmeridgian, Aptian, Albian, the Middle and Upper clastic carbonates, algal and foraminiferal assemblages Cenomanian, and the Lower Turonian. These sediments (Loftusia and Lepidorbitoides) and muddy carbonates included ammonites, some planktonic foraminiferas and with micro to cryptocrystalline dolomite which collected other pelagic and/or hemipelagic organisms. Special in a semi-restricted marine, subtidal setting. The hard sedimentological conditions led to the deposition of grounds found within the upper Simsima reflect the phosphate on the flanks of the Hamad Uplift. eustatic sea-level change which caused with the unconformity at the end of the Cretaceous. In outcrop The Hamad Uplift was a distinctive palaeostructure in (western Oman Mountains) the formation consists of the South; and the Aleppo Plateau in the north played bioclastic wackestones and packstones with abundant major roles in the distribution and differentiation of large benthic foraminifera and buildups of coral and large sedimentation during the Jurassic and Cretaceous, rudist bivalves. It can be divided into a caprinid limestone especially in the differentiation of the major structures Member, followed upward by an Orbitoidal Limestone inside the platform and on its margins. Some structural Member, both of which were deposited within a shallow activities affected the facies variations and the marine open shelf setting. sedimentation process in general, and some of them helped in conducting magma to form basaltic intrusions In subsurface, the Simsima Formation disconformably and flows, especially during the Late Jurassic, the earliest overlies the Fiqa Formation, except in southeast Abu Cretaceous and even in the Albian. Dhabi where the formation unconformably overlies the Cenomanian-Albian Shilaif, Mauddud or Nahr Umr The ophiolite complex and the associated rocks at the formations and is separated from them by a long hiatus. northwestern boundary of the Arabian platform were The top of the Simsima is marked by an unconformity emplaced in northwestern Syria (the Syrian platform), surface, which represents the end of the Cretaceous. This during the Maastrichtian. Resulting special is marked by a hiatus which separates it from the palaeogeographic conditions are represented by tectonic overlying Tertiary basal shales of the Umm Er Radhuma instability, local emersion of the transported body, Formation. It ranges in thickness from 77 to 110 meters submarine slides, and the movement of detrital debris and shows a general and gradual decrease in thickness (silici-carbonate) to the marginal African basin which from central to northwest Abu Dhabi. Towards the alternated with pelagic sedimentation and turbidites. southeast the Simsima progressively decreases in thickness until it pinches out. A prominent and consistent thinning is noticed over the structures of the producing Depositional Setting, Diagenesis and fields. This indicates that the deposition of the Simsima Reservoir Properties of the Maastrichtian was influenced by continued structural growth. In Platform Carbonate Sequences of the outcrop, the Simsima
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