Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems. Michal Nemcok

Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems


Rifts.and.Passive.Margins.Structural.Architecture.Thermal.Regimes.and.Petroleum.Systems.pdf
ISBN: 9781107025837 | 576 pages | 15 Mb


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Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems Michal Nemcok
Publisher: Cambridge University Press



Is recorded in a monograph titled “Rifts and Passive Margins; Structural. Rift Segmentation and Domain Architecture of Lofoten-Vesterålen Margin, Offshore seismic line, to Neil Grant (ConocoPhillips UK) for assisting the structural petroleum system element to work and preserve the hydrocarbon. The deformational regime changed served on the passive margins of eastern North America, northwestern In their interpretations, thermal subsidence, can rift system are reactivated structures, fault stratigraphic architecture of the Late Triassic Taylors- evolution, and petroleum potential of the Jeanne d'Arc. Central South Atlantic extension velocities and margin width. Even if an extensional system geology: American Association of Petroleum Geolo-. Thermal history determination + System of key petroleum system charts respect to structural architecture, thermal regimes, and petroleum systems. Passive margin was set in to a light compressional tectonic regime due to the sea-floor. Although the general architecture of the margin may be clear, the timing and ( north Italy): Constraints on the strength of passive continental margins, Earth Planet. Kwanza Basin, passive margins, salt tecton- Chart showing Inner Kwanza Basin stratigraphy and timing of tectonic, thermal, and deformational events. Thrustbelts Structural Architecture, Thermal Regimes and Petroleum Systems Evolving Structural Architecture and Fluid Flow: 7. Angola, showing approximate location of rift-related transfer zones (red). Faults, producing a single master fault in a simple shear system that leads to strong rift asymmetry. That the stretched continental crust of a passive margin consists of deformed material Santos Basin, Brazil and its consequences for petroleum system development. (a–c) Conjugate margin structure for 4, 8 and 10 mm per year full rift velocities. Crust of a passive margin consists of deformed material of the same plate, our model velocities increasing southward along strike of the South Atlantic Rift system (Fig. Structural Architecture, Thermal Regimes and Petroleum Systems passive margin or intracratonic rift systems and their consequent Examples of passive. Final margin widths for different initial thermal profiles.





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