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  • Geological Society of London  (2)
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  • 1
    Publication Date: 2016-10-15
    Description: The offshore Levant Basin demonstrates one of the most phenomenal natural examples of a working petroleum system associated with a relatively rapid unloading and loading cycle caused by the Messinian salinity crisis (MSC). In this study, 2D basin and petroleum systems modelling suggests that the geologically instantaneous water unloading of approximately 2070 m, and subsequent rapid salt deposition and refill, impact the subsurface pore pressure and temperature in the underlying sediments. The pressure drop is modelled to be instantaneous, whereas the impact on temperature is more of a transient response. This has important consequences for the shallow sub-Messinian biogenic petroleum system, which is assumed to have experienced fluid brecciation associated with massive fluid escape events. Deeper Oligo-Miocene sediments are far less affected, thus indicating a ‘preservation window’ for biogenic gas accumulations, which host the recent discoveries (Tamar, Leviathan, Aphrodite). Hydrocarbon accumulations of a ‘bubblepoint oil’ composition are modelled to have experienced cap expansion during the drawdown, with the pressure drop being the primary control. This study suggests that seal-limited traps are expected to have undergone a catastrophic seal failure, whereas the impact of the MSC is modelled to be less destructive for size-limited and, particularly, charge-limited traps.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
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  • 2
    Publication Date: 2016-10-15
    Description: The triggers and drivers for salt-related deformation on continental margins are intensely debated, reflecting uncertainties regarding the diagnostic value of certain structural styles, in addition to the fundamental mechanics associated with the two principal mechanisms (gliding and spreading). Determining the triggers and drivers for salt-related deformation is important because they provide insights into continent-scale geodynamic processes, the regional kinematics of gravity-driven deformation, and sediment dispersal and hydrocarbon prospectivity. The processes associated with and the timing of deformation of Messinian salt in the offshore Eastern Mediterranean are uncertain, and thus so is our understanding of the geodynamic evolution of this tectonically complex region. We here use an extensive 2D and 3D seismic reflection dataset to test models for the salt-tectonic development of Messinian salt. We contend that gliding and spreading were not mutually exclusive, but were likely to have overlapped in time and space, being associated with local and far-field tectonics (gliding), as well as differential overburden loading (spreading). We also argue that intrasalt strain and seismic-stratigraphic patterns can be explained by a model invoking a single, post-Messinian period of salt-related deformation, rather than a more complex model involving two separate deformation events that occurred during and after salt deposition.
    Print ISSN: 1354-0793
    Topics: Chemistry and Pharmacology , Geosciences
    Location Call Number Limitation Availability
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