Nd-isotopic evidence for the origin of the Sudbury complex by meteoritic impact

Details Nd-isotopic evidence for the origin of the Sudbury complex by meteoritic impact Nd-isotopic evidence for the origin of the Sudbury complex by meteoritic impact

Nov 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985jgrs...90...19f&link_type=abstract

In Lunar and Planetary Inst. 16th Lunar and Planetary Sci. Conf. p 19-23 (SEE N85-26548 15-91)

Mathematics

Logic

Copper, Meteorites, Mineral Deposits, Nickel, Rock Intrusions, Structural Properties (Geology), Canada, Geochronology, Geomorphology, Meteoritic Damage, Neodymium Isotopes

Scientific paper

A 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.

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