Fault Geometry and Deformation History, Northern Carnarvon Basin
نویسندگان
چکیده
منابع مشابه
Variation in fold geometry in the Yuso Basin, northern Spain: implications for the deformation regime
-First generation structures in greywackes of the Yuso Group from the Cantabrian Mountains of northern Spain show a distinct variation in geometry with depth in a regional synclinal structure (Curavacas and Lechada synclines); they are easily distinguished from other deformation events. In the structurally uppermost level we find 'flap folds'. Flap folds are recumbent structures with the invert...
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Figure 1. Model of P-wave velocity (above) and density (below) verses gas saturation for a sandstone reservoir with a porosity of 25%. The velocity was modelled using Gassmann’s equation (1951) with the Reuss average moduli of the fluids. For a gas saturated reservoir, a decrease in gas saturation causes a negligible change in the P-wave velocity for saturations above 20% and more significant c...
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We present a methodology to derive the growth history of a fault-tip fold above a basal detachment. Our approach is based on modeling of the stratigraphic and geomorphic records of deformation, as well as the finite structure of the fold constrained from seismic profiles. We parametrize the spatial deformation pattern using a simple formulation of the displacement field derived from sandbox exp...
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ژورنال
عنوان ژورنال: ASEG Extended Abstracts
سال: 2016
ISSN: 2202-0586
DOI: 10.1071/aseg2016ab282