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Topography and Geoid Undulations Caused By Small-Scale Convection Beneath Continental Lithosphere of Variable Elastic Thickness
Authors:Gabriele Marquart  Harro Schmeling
Affiliation:University of Uppsala, Institute of Geophysics, Department of Geodesy, Hällby, S-75590 Uppsala;University of Uppsala, Institute of Geology, Department of Mineralogy and Petrology, Box 555, S-75122 Uppsala, Sweden
Abstract:
Keywords:sublithospheric convection    continental lithosphere    elastic plate bending    topography    geoid    gravity    admittance
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