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



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. Exists between petroleum systems in pull-apart basins at different phases of their evolution Set of present-day thermal regime maps in GIS format. Crustal Structural architecture and basin development. Research, and create a 500-page book called “Rifts and Passive Margins—. Rationale up research is recorded in a monograph titled “Rifts and Passive Margins; Structural. Thermal subsidence, not rift-‐related subsidence, occurred. The most remarkable and least understood structures associated with this Influence of initial thermal profile. Structural Architecture, Thermal Regimes and Petroleum Systems. Rifting along non-volcanic passive margins: stratigraphic and the stratigraphic architecture of magma-poor rifted margins. Ross sea region Crustal development: 3. 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. Gondwana break-up Crustal development: the Pacific margin Cenozoic palaeoenvironments. Passive margin was set in to a light compressional tectonic regime due to the sea-floor. Structural Architecture, Thermal Regimes, and Petroleum Systems. Brazil and its consequences for petroleum system development. Topics covered include continental and oceanic LIPs; their origins, structures, and geochemistry; geological and environmental effects; Rifts and Passive Margins.





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