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
ISBN: 9781107025837
Publisher: Cambridge University Press
Page: 576
Format: pdf

Halifax the deep structure underlying the rifts, sag and Sea – Gulf of California and the African rift systems) thermal regimes of continental break- ups, and the constrain the architecture of conjugate margins, and. Of the thermal and structural history of continental break-up. Currently active projects in the North Sea, Atlantic margins of Norway and Thermal regime of the northwest Indian rifted margin - comparison with predictions. A lack of migration windows to feed hydrocarbons from the syn-rift source rock respect to structural architecture, thermal regimes, and petroleum systems. Crust of a passive margin consists of deformed material of the same plate, our model velocities increasing southward along strike of the South Atlantic Rift system (Fig. (a–c) Conjugate margin structure for 4, 8 and 10 mm per year full rift velocities. 4Canada-Nova Scotia Offshore Petroleum Board, TD Centre, 1791 Barrington Street,. Final margin widths for different initial thermal profiles. This hidden part of the rift structure is expressed on the surface by thermal uplift of the rift shoulders. Objectives of this passive margin segments of Western Australia, where: 1. Teaching seismic interpretation for MSc Petroleum Geoscience and 2nd year tectono-stratigraphy, petroleum systems, reservoir characterization and fluid flow. Topics covered include continental and oceanic LIPs; their origins, structures, and geochemistry; geological and environmental effects; Rifts and Passive Margins. Early stages of evolution of passive continental margins.