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Nd-isotopic evidence for the origin of the Sudbury complex by meteoritic impactA Neodymium isotopic investigation was undertaken in order to determine the possibility that the Sudbury geological structure in Ontario, Canada was formed by meteoritic impact. Conclusive evidence points to the melting of crustal rocks by way of meteoritic impact in the forming of the Sudbury structure.
Document ID
19850018243
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Faggart, B. E.
(Rochester Univ. NY, United States)
Basu, A. R.
(Rochester Univ. NY, United States)
Tatsumoto, M.
(Geological Survey Denver, United States)
Date Acquired
August 12, 2013
Publication Date
January 1, 1985
Publication Information
Publication: Lunar and Planetary Inst. 16th Lunar and Planetary Sci. Conf.
Subject Category
Lunar And Planetary Exploration
Accession Number
85N26554
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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