Add to ORKGComponents of vertical deflection as a function of anomaly potential are determined by using astrogeodetic or gravimetric methods. In this paper components of deflections obtained by astrogeodetic method were considered as conditionally correct and deflection of components determined by using gravimetric method, from conditionally correct values, were shown as digital terrain model quality functions and adopted hypothesis on the earth's crust masses density
Abstract For enhancing resolution of vertical deflections and gravity anomaly from altimetry data, a...
The gravity method is a nondestructive geophysical technique that measures differences in the earth’...
The main objective of this master thesis is random equipartition concentration of measured gravimetr...
Components of vertical deflection as a function of anomaly potential are determined by using astroge...
discovering new insights. In the field of geo-sciences, there is a wide range of mutual methods of m...
This paper compares three different methods capable of estimating the deflection of the vertical (Do...
Vertical deflection can be determined by geometrical and physical measurement. In geometrical way, v...
This paper presents the determination of the vertical deflection components using the Global Geopote...
The deflection of the vertical is an important parameter of the local gravity field which must not b...
none7siThis paper compares three different methods capable of estimating the deflection of the verti...
Recent studies on the influence of the anomalous gravity field in GNSS/INS applications have shown t...
Recent studies on the influence of the anomalous gravity field in GNSS/INS applications have shown t...
At present, information on deflections of the vertical (DOV) is obtained by means of modern global g...
The diploma introduces the local method of establishing the deflections of verticals with the help o...
Vertical gravity gradient, as a change of gravity with the change in height, is a significant physic...
Abstract For enhancing resolution of vertical deflections and gravity anomaly from altimetry data, a...
The gravity method is a nondestructive geophysical technique that measures differences in the earth’...
The main objective of this master thesis is random equipartition concentration of measured gravimetr...
Components of vertical deflection as a function of anomaly potential are determined by using astroge...
discovering new insights. In the field of geo-sciences, there is a wide range of mutual methods of m...
This paper compares three different methods capable of estimating the deflection of the vertical (Do...
Vertical deflection can be determined by geometrical and physical measurement. In geometrical way, v...
This paper presents the determination of the vertical deflection components using the Global Geopote...
The deflection of the vertical is an important parameter of the local gravity field which must not b...
none7siThis paper compares three different methods capable of estimating the deflection of the verti...
Recent studies on the influence of the anomalous gravity field in GNSS/INS applications have shown t...
Recent studies on the influence of the anomalous gravity field in GNSS/INS applications have shown t...
At present, information on deflections of the vertical (DOV) is obtained by means of modern global g...
The diploma introduces the local method of establishing the deflections of verticals with the help o...
Vertical gravity gradient, as a change of gravity with the change in height, is a significant physic...
Abstract For enhancing resolution of vertical deflections and gravity anomaly from altimetry data, a...
The gravity method is a nondestructive geophysical technique that measures differences in the earth’...
The main objective of this master thesis is random equipartition concentration of measured gravimetr...