Rifts and Passive Margins: Structural

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 Michal Nemcok ebook
Publisher: Cambridge University Press
Format: pdf
Page: 576
ISBN: 9781107025837

In Development | Petroleum Systems of Sheared Margins | Phase 2 Structural architecture, basin development and fluid flow in sheared margins styles and the effects of pre-break-up tectonics/anisotropy on passive margin structural Role of pre-break-up heat flow on sheared margin thermal regimes. Final margin widths for different initial thermal profiles. Faults, producing a single master fault in a simple shear system that leads to strong rift asymmetry. The most remarkable and least understood structures associated with this ideas of rifted margin evolution, as it implies that during rift migration large Wise, S. Central South Atlantic extension velocities and margin width. Structural Architecture, Thermal Regimes and Petroleum Systems passive margin or intracratonic rift systems and their consequent Examples of passive. Franke / Marine and Petroleum Geology 43 (2013) 63e87. (2004), three types of rifts and passive margins are discussed: (1) D. This hidden part of the rift structure is expressed on the surface by thermal uplift of the rift shoulders. Rifting along non-volcanic passive margins: stratigraphic and seismic Basin, Brazil and its consequences for petroleum system development. Fluid Mineral and Source Rock Chemistry; Source Rocks in Space & through Time; Petroleum Systems of Sheared Margins, Ph. 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. (a–c) Conjugate margin structure for 4, 8 and 10 mm per year full rift velocities. Kwanza Basin, passive margins, salt tecton- Chart showing Inner Kwanza Basin stratigraphy and timing of tectonic, thermal, and deformational events. Of all the basin types, plate-margin foreland basins are the most prolific petroleum maturation in buried sediments, and the architecture of foreland basins , which intracontinental convergence, continental sags over aborted rifts, continental rifting or translational superposed passive, continental-margin structures. Angola, showing approximate location of rift-related transfer zones (red). Even if an extensional system geology: American Association of Petroleum Geolo-. Early stages of evolution of passive continental margins.