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The shape-ratio of basin has been changed by changing the depth as well as width of the basin.
The width of the basin increases up the 130 km in its central part, the Bavarian foreland of the Alps.
It should be noted that since the seismic profile is oblique to the strike of the Tokara Channel, the actual width of the basin in the along-arc direction is much smaller.
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For the Koutavos basin case, (h) (the basin thickness) is around 80 m and (l) (the half-width of the basin) is around 500 m, which results in a shape ratio around 0.16.
In the model, the width of the attractor basins can be modulated by various factors, including the storage load.
Yet, it is largely unknown in what ways the width of confined basins and the strength of tidal currents impact sand deposition, and how this would affect reservoir architecture.
Along the low-lying North Kwanza margin, sedimentation of the broad Cenozoic to Pleistocene Kwanza submarine fan was probably governed by the width of the Kwanza interior palaeodrainage basin combined with the wet tropical Neogene climate.
A broad, shallow shelf extends up to 150 miles (240 km) in width between the mainland and the northwestern side of the basin and includes the Gulf of Tonkin and Taiwan Strait.
The peoples of the basin are diverse.
The shallow-water, shallow-basin model produces thick evaporites by continual subsidence of the basin floor.
At the nearly constant-depth part of the basin, maximum aggravation factors strongly depend on the shape ratio of the basin, defined as the ratio of the maximum thickness of the basin to its half-width.
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