Geodesy, the Concepts |
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Page 133
... lithospheric density and thickness ( including the topographical relief ) . This state of equilibrium is what the lithosphere strives for after having been depressed by the load that has subsequently been removed . There exist three ...
... lithospheric density and thickness ( including the topographical relief ) . This state of equilibrium is what the lithosphere strives for after having been depressed by the load that has subsequently been removed . There exist three ...
Page 134
... LITHOSPHERE 기 6 ° MANTLE FIG . 8.10 . Pratt's model . -UNIFORM DEPTH DM LEVEL exert the same pressure on the mantle at uniform depth D to attain an equilibrium . From this condition , the density of the continental lithosphere as a ...
... LITHOSPHERE 기 6 ° MANTLE FIG . 8.10 . Pratt's model . -UNIFORM DEPTH DM LEVEL exert the same pressure on the mantle at uniform depth D to attain an equilibrium . From this condition , the density of the continental lithosphere as a ...
Page 135
... lithospheric depth agrees fairly well with the depth determined by seismology . However , the necessity of imagining the lithosphere to be broken into independently floating blocks causes some anxiety . In reality , the lithosphere is ...
... lithospheric depth agrees fairly well with the depth determined by seismology . However , the necessity of imagining the lithosphere to be broken into independently floating blocks causes some anxiety . In reality , the lithosphere is ...
Contents
HISTORY OF GEODESY | 6 |
GEODESY AND OTHER DISCIPLINES | 20 |
STRUCTURE OF GEODESY | 46 |
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accuracy adjustment angle approximation astronomical axis azimuth C₁ called Chapter coefficients components computed considered coordinate system correction covariance matrix CT system datum defined deflection deformation denoted derived design matrix determined direction displacement earth earth's gravity field earth's surface effect ellipse equipotential surfaces error estimated evaluated filter formula frequency geocentric geodesy geodetic geoid geoidal height given global gradient gravity anomalies height differences horizontal networks integral inverse known least-squares linear lithosphere mass mathematical model mean measured meridian motion normal equations normal gravity nutation observations obtained orbital orthometric height plane plumb line polar motion position potential probability density function problem quadratic form quantities reference ellipsoid refraction relative residual satellite sea level shown in FIG solution space spherical spin statistically dependent statistically independent techniques tidal transformation unknown parameters VANÍČEK variance variations vector velocity vertical