Hypervelocity impact of steel into Coconino Sandstone

American Journal of Science
By: , and 

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Abstract

Impact of a 0.4019-g steel sphere at 4.27 km/sec into Coconino Sandstone [Permian] from Meteor Crater, Arizona, produced a crater 11-12 cm across and 2.45 cm deep. The ejecta consist of sandstone fragments, disaggregated sand, splinters of sand grains, strongly shocked aggregates of crushed sandstone grains, and chips, splinters, small amounts of silica glass, and minute spheres of steel. Part of the shocked steel was melted, and some of the melted and unmelted steel occurs as impregnations in the strongly shocked sandstone. Small amounts of glass, which were produced by shock from the sandstone, were found. The fusion of the steel cannot be due to compressive heating alone but can be partly accounted for by conduction of heat from the shocked sandstone and by production of heat by viscous drag and friction along the sandstone-projectile interface and along shear planes in the projectile.

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Publication type Article
Publication Subtype Journal Article
Title Hypervelocity impact of steel into Coconino Sandstone
Series title American Journal of Science
DOI 10.2475/ajs.261.7.668
Volume 261
Issue 7
Year Published 1963
Language English
Publisher American Journal of Science
Description 15 p.
First page 668
Last page 682
Country United States
State Arizona
Other Geospatial Coconino Sandstone, Meteor Crater
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