Introduction: The Jurassic Arab Formation is the main oil reservoir in Qatar. The Formation consists of a succession of limestone, dolomite, and anhydrite. Materials and Methods: A multi-proxy approach has been used to study the Formation. This approach is based on core analysis, thin sections, and log data in selected wells in Qatar. Results: The reservoir has been divided into a set of distinctive petrophysical units. The Arab Formation consists of cyclic sediments of oolitic grainstone/packstone, foraminifera-bearing packstone-wackestone, lagoonal mudstone and dolomite, alternating with anhydrite. The sediments underwent a series of diagenetic processes such as leaching, micritization, cementation, dolomitization and fracturing. The impa...
Pelrographic analysis of core samples of reservoir sandstones from the Sa/am Field show that porosit...
The dolostones and dolomitic limestones of the lower Cretaceous Judea formation are a key target of ...
The carbonate stringers of the Ediacaran-Early Cambrian Ara Group in the South Oman Salt Basin (SOSB...
This study is based on petrographic examination (optical, scanning electron microscope, cathodo-lumi...
An increasing need exists to quantify the impact of diagenesis on complex and heterogeneous geologic...
An increasing need exists to quantify the impact of diagenesis on complex and heterogeneous geologic...
Deposition of the Arab Formation on the Arabian Plate followed a eustatic sea-level high during the ...
The fractal fifteen thin section showed that the deposition of the Mishrif Formation is gradual upwa...
The First Eocene reservoir at the Wafra Field produces heavy oil from very porous dolomites at depth...
Five subsurface sections covering the entire length of the Jeribe Limestone Formation (Early Middle ...
International audienceThis petrographic, stable isotopic and fluid inclusion microthermometric study...
This petrographic, stable isotopic and fluid inclusion microthermometric study revealed that the dia...
Dolomitisation is a key diagenetic process, commonly improving reservoir quality in carbonate rocks....
Mesozoic and Neogene carbonates located in the Valencia Trough (offshore Spain, western Mediterranea...
Deltaic sandstones of the Middle Jurassic Brent Group, northern North Sea, have a complex diagenetic...
Pelrographic analysis of core samples of reservoir sandstones from the Sa/am Field show that porosit...
The dolostones and dolomitic limestones of the lower Cretaceous Judea formation are a key target of ...
The carbonate stringers of the Ediacaran-Early Cambrian Ara Group in the South Oman Salt Basin (SOSB...
This study is based on petrographic examination (optical, scanning electron microscope, cathodo-lumi...
An increasing need exists to quantify the impact of diagenesis on complex and heterogeneous geologic...
An increasing need exists to quantify the impact of diagenesis on complex and heterogeneous geologic...
Deposition of the Arab Formation on the Arabian Plate followed a eustatic sea-level high during the ...
The fractal fifteen thin section showed that the deposition of the Mishrif Formation is gradual upwa...
The First Eocene reservoir at the Wafra Field produces heavy oil from very porous dolomites at depth...
Five subsurface sections covering the entire length of the Jeribe Limestone Formation (Early Middle ...
International audienceThis petrographic, stable isotopic and fluid inclusion microthermometric study...
This petrographic, stable isotopic and fluid inclusion microthermometric study revealed that the dia...
Dolomitisation is a key diagenetic process, commonly improving reservoir quality in carbonate rocks....
Mesozoic and Neogene carbonates located in the Valencia Trough (offshore Spain, western Mediterranea...
Deltaic sandstones of the Middle Jurassic Brent Group, northern North Sea, have a complex diagenetic...
Pelrographic analysis of core samples of reservoir sandstones from the Sa/am Field show that porosit...
The dolostones and dolomitic limestones of the lower Cretaceous Judea formation are a key target of ...
The carbonate stringers of the Ediacaran-Early Cambrian Ara Group in the South Oman Salt Basin (SOSB...