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  • 1
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    Viscous relaxation of impact crater relief on Venus: constraints on crustal thickness and thermal gradient (1988)
    In:  J. Geophys. Res., London, Dt. Geophys. Ges. e. V., vol. 93, no. 8, 1, pp. 11911-11929, pp. L06304, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1988
    Keywords: Geothermics ; Volcanology ; Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Planetology ; JGR
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    BIBLIOGRAPHY SEISMOLOGY
  • 2
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    Penecontemporaneous metamorphism, fragmentation, and reassembly of ordinary chondrite parent bodies (1985)
    In:  Other Sources
    Details
    Publication Date: 2019-06-28
    Description: The thermal histories of ordinary chondrites and the canonical internal heating or onion shell models, which predict an inverse relation between the petrologic type of chondrites and the metallographic cooling rate, are reviewed. The thermal and accretional requirements of the 'metamorphosed planetesimal' model proposed by Scott and Rajan (1981) are analyzed, and an alternative model consistent with the metallographic cooling rate constraints is suggested in which ordinary chondrite parent bodies are collisionally fragmented and then rapidly reassembled before metamorphic heat has been dissipated.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Journal of Geophysical Research (ISSN 0148-0227); 90; 2022-202
    Format: text
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    NASA TECHNICAL REPORTS
  • 3
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    Spectral analysis of groove spacing on Ganymede (1985)
    In:  Other Sources
    Details
    Publication Date: 2019-06-28
    Description: A quantitative analysis of groove spacing on Ganymede is described. Fourier transforms of a large number of photometric profiles across groove sets are calculated and the resulting power spectra are examined for the position and strength of peaks representing topographic periodicities. The geographic and global statistical distribution of groove wavelengths are examined, and these data are related to models of groove tectonism. It is found that groove spacing on Ganymede shows an approximately long-normal distribution with a minimum of about 3.5 km, a maximum of about 17 km, and a mean of 8.4 km. Groove spacing tends to be quite regular within a single groove set but can vary substantially from one groove set to another within a single geographic region.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Journal of Geophysical Research (ISSN 0148-0227); 90; 2013-202
    Format: text
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    NASA TECHNICAL REPORTS
  • 4
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    Tectonic tests of proposed polar wander paths for Mars and the moon (1986)
    In:  Other Sources
    Details
    Publication Date: 2019-07-12
    Description: A comparison of the lithospheric stress field predicted for rapid global reorientations against observed tectonic features is used to test the polar wander paths proposed for Mars by Schultz and Lutz-Garihan (1981). A calculation of the reorientation stresses leads to the suggestion that the formation of normal faults or graben in broad regions around the former rotation poles should be the minimum tectonic signature of a reorientation that generates lithospheric stresses in excess of the extensional strength of near-surface material. It is concluded that polar wander of the magnitude and timing envisioned by Schultz and Lutz-Garihan did not occur.
    Keywords: LUNAR AND PLANETARY EXPLORATION
    Type: Icarus (ISSN 0019-1035); 65; 110-121
    Format: text
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    NASA TECHNICAL REPORTS
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