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Graben generation of major sedimentary basins
Authors:C Beaumont  JF Sweeney
Institution:1. Department of Oceanography, Dalhousie University, Halifax, N.S.Canada;2. Earth Physics Branch, Department of Energy Mines and Resources, Ottawa, Ont. K1A 0Y3 Canada
Abstract:Regional isostatic adjustment to the load that fills the trough of a large graben will produce a surface depression that extends far beyond the boundaries of the load. Sediment infilling of this depression can lead to the development of a major sedimentary basin as the regional adjustment mechanism approaches isostatic equilibrium.
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