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Title:
Seismic effects from major basin formations on the moon and Mercury
Authors:
Schultz, P. H.; Gault, D. E.
Affiliation:
AA(NASA, Ames Research Center, Space Sciences Div., Moffett Field, Calif.), AB(NASA, Ames Research Center, Space Sciences Div., Moffett Field, Calif.)
Publication:
The Moon, vol. 12, Feb. 1975, p. 159-177.
Publication Date:
02/1975
Category:
Lunar and Planetary Exploration
Origin:
STI
NASA/STI Keywords:
Lunar Maria, Mercury (Planet), P Waves, Planetary Surfaces, Seismology, Antipodes, Impact Damage, Lunar Craters, Moonquakes, Spallation, Terrain Analysis
Comment:
; AAA013.094.236
DOI:
10.1007/BF00577875
Bibliographic Code:
1975Moon...12..159S

Abstract

Grooved and hilly terrains occur at the antipode of major basins on the moon (Imbrium, Orientale) and Mercury (Caloris). Such terrains may represent extensive landslides and surface disruption produced by impact-generated P-waves and antipodal convergence of surface waves. Order-of-magnitude calculations for an Imbrium-size impact on the moon indicate P-wave-induced surface displacements of 10 m at the basin antipode that would arrive prior to secondary ejecta. Comparable surface waves would arrive subsequent to secondary ejecta impacts beyond 1000 km and would increase in magnitude as they converge at the antipode. Other seismically induced surface features include: subdued, furrowed crater walls produced by landslides and concomitant secondary impacts; emplacement and leveling of light plains units owing to seismically induced 'fluidization' of slide material; and perhaps the production and enhancement of deep-seated fractures that led to the concentration of farside lunar maria in the Apollo-Ingenii region.

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