TAILIEUCHUNG - .New Frontiers in Integrated Solid Earth Sciences Phần 6

Những thành tựu và thách thức trong lưu vực trầm tích Dynamics Hình. 43 Hậu quả của sự hiện diện hay vắng mặt của các khu điểm yếu của vỏ trái đất thấp hơn về nội địa hoá biến dạng thạch quyển mở rộng. | Achievements and Challenges in Sedimentary Basins Dynamics 203 Fig. 43 Consequences of presence or absence of lower crustal weakness zones on localization of deformation in extended lithosphere. a Increase of width of deformed zone during ongoing extension b Planview of extending lithosphere for two end-member models model incorporating lower crustal weakness zone WLC top model without crustal weakness zone bottom from Corti et al. 2003 passive margins foreland basins and foothills domains. Geological processes operating in sedimentary basins are too complex to be addressed by a single multiprocess numerical tool. Therefore it is quite important to generate easy-access databases and to allow for the import and export of files from one code to the other in order to develop interactive workflows and more integrated approaches. Moreover allowance must be made for switching back and forth between basin-scale and reservoir-scale studies. In the following we describe such an integrated workflow which couples analytical work and Volcanics Future SDRs Cross section in the south Future break-up Evolution through time on top views Fig. 44 Application of rifted continental margin of Mid-Norway from Sokoutis et al. 2007 204 F. Roure et al. modelling and addresses the interactions between selected but complex geological processes operating at various temporal and spatial scales in sedimentary basins. Dynamic Controls on Reservoir Quality in Foreland Fold-and-Thrust Belts Integration of various datasets ranging from seismic profiles to thin-sections analytical work and modelling is a prerequisite for the appraisal of sub-thrust sandstone reservoirs the porosity-permeability evolution of which results from mechanical and chemical compaction both processes interacting in response to sedimentary burial horizontal tectonic stress and temperature. First results of the SUBTRAP SUB-Thrust Reservoir Appraisal consortium studies have shown that in the Sub-Andean basins of Venezuela and .

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