The role of volatiles and lithology in the impact cratering process.
Reviews of Geophysics and Space Physics
By: Kieffer S. Werner and C.H. Simonds
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Abstract
A survey of published descriptions of 32 of the largest, least eroded terrestrial impact structures reveals that the amount of melt at craters in crystalline rocks is approximately 2 orders of magnitude greater than at craters in sedimentary rocks. In this paper we present a model for the impact process; calculations show that the volume of material shocked to pressures sufficient for melting should not be significantly different in sedimentary and crystalline rocks. We conclude that shock melt is formed in the early stages of the cratering process by impacts into rocks rich in volatiles but is destroyed by the cratering process. -from Authors
Suggested Citation
Werner, K.S., Simonds, C., 1980, The role of volatiles and lithology in the impact cratering process.: Reviews of Geophysics and Space Physics, v. 18, no. 1, p. 143-181, https://doi.org/10.1029/RG018i001p00143.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | The role of volatiles and lithology in the impact cratering process. |
| Series title | Reviews of Geophysics and Space Physics |
| DOI | 10.1029/RG018i001p00143 |
| Volume | 18 |
| Issue | 1 |
| Publication Date | June 14, 2010 |
| Year Published | 1980 |
| Language | English |
| Publisher | American Geophysical Union |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Reviews of Geophysics and Space Physics |
| First page | 143 |
| Last page | 181 |