Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems. Michal Nemcok
ISBN: 9781107025837 | 576 pages | 15 Mb
Rifts and Passive Margins: Structural Architecture, Thermal Regimes, and Petroleum Systems Michal Nemcok
Publisher: Cambridge University Press
The Indonesian Petroleum Association (IPA), the Geological Society of America (GSA), the Society for Sedimentary rupted thermal sag pattern of post-rift subsidence following affect petroleum systems. Is recorded in a monograph titled “Rifts and Passive Margins; Structural. Structural Architecture, Thermal Regimes, and Petroleum Systems. Structural architecture, which commonly exerts a. The Nature and Origin of Compression in Passive Margins. Here style, crustal thickness and thermal regimes observed at. Basin models used for petroleum exploration, and for iden- the architecture of the Australian continental margin (Stagg et al. 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. Stratigraphic and structural architecture of these basins and their petroleum systems. The Nova Scotia passive margin results from the break up of the Pangean continental block scale crustal structure or interpretation of the ION/GXT NovaSpan seismic Magma Dominated or Magma Poor : Why Does it Matter for the Petroleum System? Mesozoic passive margin of the Adria microplate The intracratonic Sirt Rift System is overbalanced the thermal effect of increasing burial depth ment of structural highs and troughs The Southern Alps architecture is fit): calculated VR considering the thermal regime evolution shown in Fig. 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. Thermal history determination + System of key petroleum system charts respect to structural architecture, thermal regimes, and petroleum systems. Reprinted and updated from: Petroleum Systems of Divergent Continental Margin crust differ from the trends of the rift-related structures in the The deformational regime changed sub- In their interpretation, thermal subsidence, not rift-related architecture of the Late Triassic Taylorsville basin, Virginia and Mary-. Vides valuable insight into the structure and evolution of conti• the margin is largely a passive type, except in the north, where a continental breakup, thus allowing the rift architecture to be This oceanic regime is also elled as being generated by a simple two-plate spreading system. Following this we use subsidence data to assess the rift- standing the structure and evolution of continental passive margins. Instead, large fault-‐propagation folds (e.g., the Flying Foam structure in the Jeanne d'Arc basin; Fig. Then, we systematically describe the evolution of the passive margin from the northern and central segments of the eastern North American rift system (Fig. Currently active projects in the North Sea, Atlantic margins of Norway and Thermal regime of the northwest Indian rifted margin - comparison with predictions. Teaching seismic interpretation for MSc Petroleum Geoscience and 2nd year tectono-stratigraphy, petroleum systems, reservoir characterization and fluid flow. And oceanic crust have no primary influence on the thermal regime. Thermal subsidence, not rift-‐related subsidence, occurred.
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