Floor‐fractured crater models of the Sudbury Structure, Canada: Implications for initial crater size and crater modification
- 15 June 1993
- journal article
- Published by Wiley in Meteoritics
- Vol. 28 (2) , 222-231
- https://doi.org/10.1111/j.1945-5100.1993.tb00760.x
Abstract
No abstract availableKeywords
This publication has 22 references indexed in Scilit:
- Osmium isotope evidence for a crustal origin of platinum group elements in the Sudbury nickel ore, Ontario, CanadaGeochimica et Cosmochimica Acta, 1992
- The Sudbury structure: Controversial or misunderstood?Journal of Geophysical Research, 1991
- Strontium- and neodymium-isotopic characteristics of a heterolithic breccia in the basement of the Sudbury impact structure, CanadaEarth and Planetary Science Letters, 1989
- Origin of the Sudbury Complex by Meteoritic Impact: Neodymium Isotopic EvidenceScience, 1985
- Lunar floor‐fractured craters: Evidence for viscous relaxation of crater topographyJournal of Geophysical Research, 1981
- Manicouagan Impact Melt, Quebec, 1, Stratigraphy, petrology, and chemistryJournal of Geophysical Research, 1978
- Modification of premare impact craters by volcanism and tectonismEarth, Moon, and Planets, 1975
- Impact meltsJournal of Geophysical Research, 1971
- Possible relations between meteorite impact and igneous petrogenesis, as indicated by the Sudbury structure, Ontario, CanadaBulletin of Volcanology, 1970
- Rille pattern in the lunar crater HumboldtJournal of Geophysical Research, 1968