Gravity, Geoid and Marine Geodesy: International Symposium No. 117 Tokyo, Japan, September 30 - October 5, 1996
Based on an international symposium held in Tokyo, the volume combines papers in the fields of gravity, geoid and marine geodesy. Special emphasis is placed on the use of gravity in modeling tectonic processes and the problems of geophysical inversion. In addition, absolute and relative gravity measurement in static and airborne mode, satellite altimetry, geopotential modeling, and global geodynamics are dealt with. The field of marine geodesy includes contributions on sea level change, seafloor deformation and mapping, sea surface positioning, electronic charting, and datum transformations.
1116787488
Gravity, Geoid and Marine Geodesy: International Symposium No. 117 Tokyo, Japan, September 30 - October 5, 1996
Based on an international symposium held in Tokyo, the volume combines papers in the fields of gravity, geoid and marine geodesy. Special emphasis is placed on the use of gravity in modeling tectonic processes and the problems of geophysical inversion. In addition, absolute and relative gravity measurement in static and airborne mode, satellite altimetry, geopotential modeling, and global geodynamics are dealt with. The field of marine geodesy includes contributions on sea level change, seafloor deformation and mapping, sea surface positioning, electronic charting, and datum transformations.
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Gravity, Geoid and Marine Geodesy: International Symposium No. 117 Tokyo, Japan, September 30 - October 5, 1996
747
Gravity, Geoid and Marine Geodesy: International Symposium No. 117 Tokyo, Japan, September 30 - October 5, 1996
747Paperback(Softcover reprint of the original 1st ed. 1997)
$329.00
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329.0
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Product Details
ISBN-13: | 9783642083280 |
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Publisher: | Springer Berlin Heidelberg |
Publication date: | 12/03/2010 |
Series: | International Association of Geodesy Symposia , #117 |
Edition description: | Softcover reprint of the original 1st ed. 1997 |
Pages: | 747 |
Product dimensions: | 8.27(w) x 10.98(h) x 0.06(d) |
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