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  • 1
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    Evidence from satellite altimetry for small-scale convection in the mantle (1985)
    In:  CASI
    Details
    Publication Date: 2016-06-07
    Description: Small scale convection can be defined as that part of the mantle circulation in which upwellings and downwellings can occur beneath the lithosphere within the interiors of plates, in contrast to the large scale flow associated with plate motions where upwellings and downwellings occur at ridges and trenches. The two scales of convection will interact so that the form of the small scale convection will depend on how it arises within the large scale flow. Observations based on GEOS-3 and SEASAT altimetry suggest that small scale convection occurs in at least two different ways.
    Keywords: GEOPHYSICS
    Type: NASA, Washington Geopotential Res. Mission (GRM); p 69-70
    Format: application/pdf
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    NASA TECHNICAL REPORTS
  • 2
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    Gravity, geoid and the oceanic lithosphere (1985)
    In:  CASI
    Details
    Publication Date: 2016-06-07
    Description: Plate tectonics and its contribution to progress in studies of the Earth's gravitational field is discussed. In acquisition, the development of forced feedback accelerometers, satellite navigation, and satellite radar altimetry significantly improved the accuracy and coverage of gravity data over the oceans. In interpretation, gravity and geoid anomalies are used to determine information on the thermal and mechanical properties of the oceanic lithosphere and the forces that drive plate motions.
    Keywords: GEOPHYSICS
    Type: NASA, Washington Geopotential Res. Mission (GRM); p 28
    Format: application/pdf
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    NASA TECHNICAL REPORTS
  • 3
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    The relationship between gravity and bathymetry in the Pacific Ocean (1985)
    In:  Other Sources
    Details
    Publication Date: 2019-07-12
    Description: The study of the earth's gravitational field has provided one of the principal methods for the determination of the structure of the outer layers of the earth. A project has been undertaken which involves the systematic examination of the relationship between the earth's gravity field and topography in each of the earth's major ocean basins. The first part of the project was concerned with the compilation, reduction, and analysis of the available surface-ship gravity and bathymetry and satellite-derived geoid data in the oceans of the earth. The present paper has the objective to summarize the principal results which have been obtained so far in the Pacific Ocean.
    Keywords: GEOPHYSICS
    Type: AD-A163260 , Geophysical Journal (ISSN 0016-8009); 83; 263-298
    Format: text
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    NASA TECHNICAL REPORTS
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