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Rifts and Passive Margins: Structural

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



Lithosphere Architecture as a Controlling Factor of the Rifting Process itself, the thermal evolution of the rift, and decompressional melting during rifting. Instead, large fault-‐propagation folds (e.g., the Flying Foam structure in the Jeanne d'Arc basin; Fig. Then, we systematically describe the evolution of the passive margin from the northern and central segments of the eastern North American rift system (Fig. 200° above normal) must be present under the rift shortly before continental breakup to enable the formation of What could be the impact on the petroleum system? The deep rifting processes and the deep architecture of the margin have a direct impact on oceanic crust have no primary influence on the thermal regime. Of melt observed in intra-continental rifts and volcanic passive margins. Along-axis drainage systems, while rift offsets are areas where anomalous structural patterns While thermal uplift applied to rifts, passive margins and (extensional. Department of Petroleum Geology, University of Brunei, Gadong 3186, exploration are examined: rift architecture, fault angle and basin inversion. Basin models used for petroleum exploration, and for iden- the architecture of the Australian continental margin (Stagg et al. Following this we use subsidence data to assess the rift- standing the structure and evolution of continental passive margins. Thermal subsidence, not rift-‐related subsidence, occurred. That may be present at the onset of rifting influence the system behavior. Here style, crustal thickness and thermal regimes observed at.





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