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In this paper, some features of conducting experiments on core samples to determine mechanical properties were established. Detailed description for such type of testing is poorly described in regulatory documents (Russian State Standard, ASTM). Problem of specific test methods selection in accordance to task before the geomechanical modeling is considered. For the most issues, a series of experiments to build a failure envelope is required. Details of sample preparation for compression tests are regarded. In particular, the advantages and disadvantages of different methods for preserving in-situ core saturations are discussed: the collection of an isolated core with subsequent conservation or the preparatory work with the extraction, drying and saturation of samples. While conducting multi-stage compression tests for building Mohr circles, chose of the right moment to stop the loading stage has a significant effect to prevent destruction of the sample in the early stages. This paper demonstrated that for specimens characterized by a shear failure type, it is recommended to focus on the plot "axial stress - volumetric strain". In particular, the inflection point of the curve, that is the moment of reaching the maximum value of volumetric deformation could be selected as a criterion for the loading stage termination. For samples with high porosity, a complete testing cycle to build the Mohr circles and the entire failure curve is given.
In this paper, some features of conducting experiments on core samples to determine mechanical properties were established. Detailed description for such type of testing is poorly described in regulatory documents (Russian State Standard, ASTM). Problem of specific test methods selection in accordance to task before the geomechanical modeling is considered. For the most issues, a series of experiments to build a failure envelope is required. Details of sample preparation for compression tests are regarded. In particular, the advantages and disadvantages of different methods for preserving in-situ core saturations are discussed: the collection of an isolated core with subsequent conservation or the preparatory work with the extraction, drying and saturation of samples. While conducting multi-stage compression tests for building Mohr circles, chose of the right moment to stop the loading stage has a significant effect to prevent destruction of the sample in the early stages. This paper demonstrated that for specimens characterized by a shear failure type, it is recommended to focus on the plot "axial stress - volumetric strain". In particular, the inflection point of the curve, that is the moment of reaching the maximum value of volumetric deformation could be selected as a criterion for the loading stage termination. For samples with high porosity, a complete testing cycle to build the Mohr circles and the entire failure curve is given.
Advanced rock mechanical characterization of a giant Cretaceous carbonate field in Abu Dhabi is the focus of this paper, that not only focused on routine triaxial tests for shear strength estimates but also to understand pore collapse, tensile strength, thermal and creep behavior of these rocks. The approach has started with auditing and selection of core intervals from various offset wells. These core intervals are selected to represent lateral and vertical coverage of various sub-units within various reservoir and caprock intervals. Scratch tests and whole core CT scans are conducted for selection of appropriate intervals for extracting core plugs. Specialized techniques are deployed for plugging the core intervals. Pre and post-test photographs and CT scans of all the plugs are taken to identify the role of heterogeneity. The testing program encompasses various triaxial tests such as single stage (SST), multi-stage (MST), and unconfined compressive strength (UCS) tests. They are crucial for understanding rock shear failure, strength parameters like UCS, cohesion, friction angle, and stiffness properties including Young's modulus and Poisson's ratio. Acoustic velocity is also recorded during these tests. Additionally, tests like uniaxial pore volume compressibility (UPVC) and Biot are performed to ascertain the compressibility and poro-elastic coefficients. Hydrostatic compaction tests provide insights into pore collapse onset, while Brazilian tests measure tensile strength, and fracture toughness tests assess resistance to crack growth. We also conduct thermal expansion and creep tests to determine the rocks’ thermal behaviour and time-dependent deformation characteristics. Based on the results of rock mechanics testing program, mechanical rock properties correlations have been developed for various reservoir units and caprock. These correlations demonstrate a relationship between geomechanical and petrophysical properties. The developed bespoke correlations have been successfully used across different wells, demonstrating accurate core-log calibrations of mechanical rock properties. This high-level characterization of carbonate reservoirs and caprocks aid in comprehending rock behavior under various field development conditions: such as reservoir depletion, fluid injection, potential CO2 sequestration, and modeling of thermal and creep phenomena.
Oman Mountains deformation is being continued by massive thrust fault systems in Eastern Abu Dhabi basins with dissipating stresses laterally to the subsurface. Thrust faults with a strike-slip component that include a fault damage zone of strong rock shearing, and complicated zones of deformation. The initial episode was caused by the compressional movement of the Masirah, which faulted and folded again during the Semail tectonic events. Large faults are typically modelled on seismic as a single, large slip plane, but the outcrop analogues demonstrate the case is far more intricate, according to understanding of fault zone complexity and fault rock attributes. To understand the strength characteristics and seismic behaviour of faults in the subsurface, more in-depth information of the growth and structural style of thrust systems on outcrop analogues is essential considering the future exploration in eastern Abu Dhabi. Architecture, geometry, and tectonic uplift resulting from accumulated slip on the faults are all expressed at the surface that can express the geometrical prediction in subsurface. The paper describes the geological features and evidence of inversion structures, such as anticlines, reverse faults, and detachment surfaces, using seismic data, well logs, and surface outcrop analogues. It also explains the kinematic models, strain rates, and restoration methods used to understand the structural evolution and deformation history of the region. It highlights the positive and negative effects of inversion tectonics on hydrocarbon generation, migration, and trapping, and how they vary depending on the fault orientation, lithology, fluid pressure, and tectonic context. It suggests that the Abu Dhabi basin has experienced multiple phases of extension and compression, resulting from the interaction of the Arabian and Eurasian plates, and that the strike-slip faulting regime has played a significant role in shaping the basin geometry and hydrocarbon potential. This study has provided new insights into the geometry, timing, and driving mechanisms of thrusting deformation, as well as the regional tectonic implications of the fold-thrust belt. The fold-thrust belt can be further divided into three sub-belts, including the Northern Emirates zone, the eastern Abu Dhabi and the Abu Dhabi basin including onshore fields and further west. The former is characterized by imbricate stepped-thrust sheets composed of developed thrusts and related folds, and the detachment-fold sub-belt, which is composed of box, chevron, and closed overturned-isoclinal folds. The second eastern Abu Dhabi zone is characterized by thrust-fold sub-belt observed on seismic. The last western zone is mainly showing strike slip regime with few thrusts zones, which may due the transpressional regime between the fault segments.
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