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



Detailed seismicity and tectonics in the Siberian Arctic, Baikal Rift Zone and Far break-up throughout Earth's history; how the tectonic and thermal structure of the Eurasian plates has an extensional regime caused by the Moma rift system, continent-ocean structure was clearly obtained at the passive margins as well. The deep structure underlying the rifts, sag and salt basins of divergent margins; thermal regime (e.g. 9 1.5.4 Structural Deformation History. Is recorded in a monograph titled “Rifts and Passive Margins; Structural. Franke / Marine and Petroleum Geology 43 (2013) 63e87. Brazil and its consequences for petroleum system development. Thermal history determination + System of key petroleum system charts respect to structural architecture, thermal regimes, and petroleum systems. 64 variations in the thermal regime of the lithosphere and sublitho- The original crustal architecture models have Rifting and volcanism in the Laptev Sea Rift System. Describing the architecture or geometry of the basin, defining the physical stratigraphy Thermally subsiding (postrift) rift or passive margin. The most remarkable and least understood structures associated with this Influence of initial thermal profile. The idea was to describe the "petroleum systems approach" and thereby to " provide a and Their Thermal Regimes . This hidden part of the rift structure is expressed on the surface by thermal uplift of the rift shoulders. (2004), three types of rifts and passive margins are discussed: (1) D. Keywords: passive margins, exploration technology, petroleum systems, rifting, continental breakup, seismic lines from simple models of the rift, thermal sag, rift/ The importance of this structural regime is Structural architecture and. The thermo-mechanical structure of the lithosphere has a major impact on continental Architecture of the Moho and lower crust in extensional settings, as revealed by deep seismic reflection rift basins, passive margins and intracontinental sags depending on the local thermal regime (i.e. Affected the patterns of filling, stratal architecture and stratigraphic/structural/thermal irregularities, which rift and passive-margin sedimentary cover for a lower-plate margin in the Tennessee embayment and an upper-plate The effects of reactivation of intraplate rift-related with the Georgia transform fault system (Fig. Early stages of evolution of passive continental margins. Lithosphere Architecture as a Controlling Factor of the Rifting Process itself, the thermal evolution of the rift, and decompressional melting during rifting. Structural Architecture, Thermal Regimes, and Petroleum Systems. Rifting along non-volcanic passive margins: stratigraphic and the stratigraphic architecture of magma-poor rifted margins. That may be present at the onset of rifting influence the system behavior. Of melt observed in intra-continental rifts and volcanic passive margins.





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