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Ar-40 to Ar-39 dating of pseudotachylites from the Witwatersrand basin, South Africa, with implications for the formation of the Vredefort DomeThe formation of the Vredefort Dome, a structure in excess of 100 km in diameter and located in the approximate center of the Witwatersrand basin, is still the subject of lively geological controversy. It is widely accepted that its formation seems to have taken place in a single sudden event, herein referred to as the Vredefort event, accompanied by the release of gigantic amounts of energy. It is debated, however, whether this central event was an internal one, i.e., a cryptoexplosion triggered by volcanic or tectonic processes, or the impact of an extraterrestrial body. The results of this debate are presented.
Document ID
19930001001
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Trieloff, M.
(Max-Planck-Inst. fuer Kernphysik Heidelberg, Germany)
Kunz, J.
(Max-Planck-Inst. fuer Kernphysik Heidelberg, Germany)
Jessberger, E. K.
(Max-Planck-Inst. fuer Kernphysik Heidelberg, Germany)
Reimold, W. U.
(Witwatersrand Univ. Johannesburg, South Africa)
Boer, R. H.
(Witwatersrand Univ. Johannesburg, South Africa)
Jackson, M. C.
(Witwatersrand Univ. Johannesburg, South Africa)
Date Acquired
September 6, 2013
Publication Date
January 1, 1992
Publication Information
Publication: Lunar and Planetary Inst., International Conference on Large Meteorite Impacts and Planetary Evolution
Subject Category
Geophysics
Accession Number
93N10189
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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