By Makhous, Monzer; Galushkin, Yu. I.
This e-book is dedicated to the sector of basin research, and specifically to the single- and two-dimensional modeling of the burial, thermal and maturation histories of sedimentary basins, within the context of comparing their hydrocarbon capability. a brand new modeling procedure is elaborated during this paintings and utilized to continental basins. specific consciousness is paid to precise positive factors of basin evolution, together with the compaction of sediments deposited at a variable cost, erosion of the sedimentary strata and basement, intrusive and hydrothermal task, thermal activation and reactivation of the basement, lateral warmth trade of multiple-aged blocks of the oceanic and continental lithospheres, the leaping of spreading axes, and so forth. substitute equipment are utilized for the regulate of tectonic subsidence, isostasy and rheology, lithosphere stretching and thinning.
desk of Contents
1. The Geodynamic atmosphere and a few Geomechanical facets of the Initiation and Evolution of Rift Basins
2. Numerical Reconstruction of the Burial and Thermal Histories of Sedimentary Basins within the computing device Galo approach for Basin Modeling: major ideas of the procedure
three. Numerical Reconstruction of the conclusion of Hydrocarbon capability of resource Rocks in the course of Basin's Burial background
four. research of Continental Sedimentary Basins within the Galo Modeling method
five. research of the Basins of Continental Passive Margins and Back-Arc facilities: Geodynamics, Thermal and Maturation Histories
record of Figures
record of Tables
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Additional resources for Basin Analysis and Modeling of the Burial, Thermal and Maturation Histories in Sedimentary Basins
Therefore, an alternative eclogite mechanism for basin subsidence has been proposed. Only this mechanism can explain the fast submerging of the Black Sea in Eocene-Quaternary (1–2 km) without visible distortions of the sedimentary cover by faults in this time [Artyushkov, 1992]. Occasionally, these basins are lacking in features typical of the regional uplift prior to the onset of basin subsidence as well as in features associated with the thinning of the lithosphere. Finally, the subsidence of these basins fails to obey the thermal law t [Flower and Nisbet, 1985].
The extension amplitude involved in the generation of such a cleft and continental break was found to be linearly related to the length of the pre-existing weakened zone, which makes it possible to gain insight into the length distribution and mutual orientation (in plane) of individual areas of passive continental margins [Dunbar and Sawyer, 1996]. It was reported in a number of works that such zones of lithospheric weakening might be quasi-stationary in character, so that the repeating events of opening and closing of ocean basins (Wilson cycle) roughly occur along the same lineaments [Ryan and Dewey, 1997].
1. 5 Basins in the Pre-Orogenic, Early Orogenic and Post-Orogenic Stages of Lithosphere Evolution Transition to the next stage — complete closure of the oceanic trough owing to the collision of the continental edges of the lithospheric plates accompanied by orogeny — is effected gradually, in steps. It extends over a prolonged period during which multiple collisions on a smaller scale take place involving passive margins, island arcs, chains of sea mountains and microcontinents (modern boundary between the Australian and EuroAsian plates).
Basin Analysis and Modeling of the Burial, Thermal and Maturation Histories in Sedimentary Basins by Makhous, Monzer; Galushkin, Yu. I.