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Science 22 July 1960: Vol. 132. no. 3421, pp. 220 - 222 DOI: 10.1126/science.132.3421.220
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Articles
First Natural Occurrence of Coesite
E. C. T. Chao 1,
E. M. Shoemaker 1, and
B. M. Madsen 1
1 U.S. Geological Survey, Washington, D.C.
Coesite, the high-pressure polymorph of SiO2, hitherto known only as a synthetic compound, is identified as an abundant mineral in sheared Coconino sandstone at Meteor Crater, Arizona. This natural occurrence has important bearing on the recognition of meteorite impact craters in quartz-bearing geologic formations.
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192, 17-57
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- Rheology of planetary lithospheres: a review from impact cratering mechanics.
- P. G. Thomas, P. Allemand, and N. Mangold (1997)
Geological Society, London, Special Publications
121, 39-62
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- Terrestrial catastrophism: causes and effects.
- R. J. Huggett and R.J. Huggett (1988)
Progress in Physical Geography
12, 509-532
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- Sudbury Structure, Ontario: Some Petrographic Evidence for Origin by Meteorite Impact.
- B. M. French and B. M. French (1967)
Science
156, 1094-1098
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- Coesite Discovered in Tektites.
- L. S. Walter and L. S. Walter (1965)
Science
147, 1029-1032
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- Stishovite: Thermal Dependence of the Crystal Habit.
- C. B. Sclar, C. B. Sclar, L. C. Carrison, and G. G. Cocks (1964)
Science
144, 833-835
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