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Origin of the Vredefort structure, South Africa: Impact modelA model is presented for the evolution of the Vredefort structure, based on reasoned constraints on the original size of the Vredefort structure from observational data and comparison with other terrestrial impact craters. The models for complex craters (ring and multi-ring basins) of Croft, Grieve, and co-workers, and Schultz and co-workers, were used to reconstruct the Vredefort impact event, using a final crater diameter of 300 km, as estimated by Therriault. The sequence of events (stages 2-5) is illustrated diagramatically. The stages are: initial penetration, excavation and compression, dynamic rebound and uplift, maximum radial growth and collapse, and final crater form.
Document ID
19940016353
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Therriault, A. M.
(Houston Univ. TX, United States)
Reid, A. M.
(McMaster Univ. Hamilton, Ontario., Canada)
Reimold, W. U.
(Witwatersrand Univ. Johannesburg, South Africa)
Date Acquired
September 6, 2013
Publication Date
January 1, 1993
Publication Information
Publication: Lunar and Planetary Inst., Twenty-Fourth Lunar and Planetary Science Conference. Part 3: N-Z
Subject Category
Geophysics
Accession Number
94N20826
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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