Multi-ring basin formation - Possible clues from impact cratering calculationsFinite difference continuum mechanics code calculations make it possible to vary the controlling variables in an impact event and to determine basic trends at scales unavailable to experimental analysis. Orphal et al. (1980) have summarized the results of a pair of such calculations for identical projectile/target characteristics but different impact velocities. One calculation considered a relatively low velocity iron impactor (5 km/s); the other, a high velocity iron impactor (15.8 km/s). The primary purpose was to investigate the generation and transport of impact melt for the two impact energies. Attention is given to crater growth, crater ejecta, and possible implications for basin-size events. Based on extrapolations, a new scenario is proposed. The scenario incorporates elements of several existing basin models.
Document ID
19820055513
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Schultz, P. H. (Lunar and Planetary Inst. Houston, TX, United States)
Miller, B. (Lunar and Planetary Institute Houston, TX, United States)
Orphal, D. (Lunar and Planetary Inst. Houston, TX, United States)
Borden, W. F. (Lunar and Planetary Inst. Houston, TX, United States)
Larson, S. A. (California Research and Technology, Inc. Livermore, CA, United States)
Date Acquired
August 10, 2013
Publication Date
January 1, 1981
Subject Category
Lunar And Planetary Exploration
Meeting Information
Meeting: Multi-ring basins: Formation and evolution