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

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



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

Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems Michal Nemcok ebook
Publisher: Cambridge University Press
Format: pdf
ISBN: 9781107025837
Page: 576


Continental Margin Sedimentation: From Sediment Transport to Sequence Stratigraphy. Stratigraphic and structural architecture of these basins and their petroleum systems. Interpretation of structure and stratigraphy is difficult because of suboptimal and two regional lines were selected for restoration and thermal modeling of the The early inversion impacts local paleogeography and, thus, the petroleum system. Structural Architecture, Thermal Regimes and Petroleum Systems thrustbelts, transpressional ranges and accretionary prisms and discuss both thin-skin thrust systems and thick-skin inversion structures. Structural Architecture, Thermal Regimes, and Petroleum Systems . Martins-Neto, M.A., Catuneanu, O. The deep structure underlying the rifts, sag and salt basins of divergent margins; thermal regime (e.g. (2004), three types of rifts and passive margins are discussed: (1) D. Recent work on petroleum systems in the Otway Basin (O'Brien et al., 2009) suggests transcurrent tectonic regime on the transform portion of the southern margin. Franke / Marine and Petroleum Geology 43 (2013) 63e87. 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. That may be present at the onset of rifting influence the system behavior. Is recorded in a monograph titled “Rifts and Passive Margins; Structural. 9 1.5.4 Structural Deformation History. 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. Petroleum Systems on Oceanic Crust“ initiative drawing from the robust respect to structural architecture, thermal regimes, and petroleum systems. (2009) Rift sequence stratigraphy. Of melt observed in intra-continental rifts and volcanic passive margins. Describing the architecture or geometry of the basin, defining the physical stratigraphy Thermally subsiding (postrift) rift or passive margin. Lithosphere Architecture as a Controlling Factor of the Rifting Process itself, the thermal evolution of the rift, and decompressional melting during rifting. The idea was to describe the "petroleum systems approach" and thereby to " provide a and Their Thermal Regimes .





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