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



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. Fluid Mineral and Source Rock Chemistry; Source Rocks in Space & through Time; Petroleum Systems of Sheared Margins, Ph. 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. (2004), three types of rifts and passive margins are discussed: (1) D. A lack of migration windows to feed hydrocarbons from the syn-rift respect to structural architecture, thermal regimes, and petroleum systems. Franke / Marine and Petroleum Geology 43 (2013) 63e87. 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. Early stages of evolution of passive continental margins. This hidden part of the rift structure is expressed on the surface by thermal uplift of the rift shoulders. Structural architecture maps with indication of break-up trajectory advance with time along both passive margin segments of Western Australia, where: 1.





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