--> --> Lateral Mobility of Minibasins During Shortening: Insights From the SE Precaspian Basin, Kazakhstan

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Lateral Mobility of Minibasins During Shortening: Insights From the SE Precaspian Basin, Kazakhstan


Minibasin provinces are widespread and can be found in all types of salt-tectonic settings, many of which are prone to shortening. Previous studies of how minibasin provinces shorten assume that the salt between the minibasins is homogeneous and that the base of salt is flat or of low relief, such that minibasins are free to move laterally. In this presentation we investigate how minibasin provinces respond to shortening when the lateral mobility of the minibasins is restricted by intra-salt sediment bodies, in order to gain a greater understanding of the controls on the structural styles and modes of tectono-stratigraphic evolution exhibited in minibasin provinces. We examine a borehole-constrained, 3D seismic reflection dataset from the SE Precaspian Basin (onshore western Kazakhstan). The study area is characterised by large, supra-salt minibasins of Late Permian to Late Triassic age and an array of smaller, intra-salt sediment packages of Late Permian age that lie in the salt between the larger minibasins. We first outline the evidence of episodic shortening between the Late Triassic and present, after the onset of supra-salt minibasin subsidence. Next, we document spatial variations in shortening style, showing how these relate to variations in the concentration of intra-salt sediment packages. Finally, we develop synoptic models showing how intra-salt sediment packages influence both the lateral mobility of minibasins during shortening and the resultant structural style. We compare and contrast our findings with existing models and natural examples of shortened minibasin provinces, with particular focus on their applicability to the Gulf of Mexico. We conclude that minibasin provinces have different degrees of lateral mobility and that these variations provide a first-order control on basin-shortening style and tectono-stratigraphic evolution.