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- W1632660206 abstract "The computation of the anomalous gravity field at points placed above the relief as a function of its observed values on the irregular topographical surface is of particular importance both in gravity prospecting, (Henderson and Cordell, 1971), (Bhattacharyya and Chan, 1977), (Hansen and Miyazaki, 1984) and physical geodesy, (Molodensky, Eremeev and Yurkina, 1960), (Heiskanen and Moritz, 1967). The upward continuation represents a high accurate low-pass filter with a meaningful output in geophysical terms, allowing one to compare surface measurements to airborne or satellite data. Computation of the derivatives of the field at various elevations can be easily performed too. In this paper, a high accurate boundary element procedure derived by Ivan (1994) to process gravity data acquired on a quasi-plane surface is modified to take into account the curvature of the Earth. The possibility to obtain the anomalous potential above the topographic surface from unevenly spaced Bouguer anomaly is discussed.KeywordsGravity FieldBouguer AnomalyContour IntervalPhysical GeodesyPolyhedral SurfaceThese keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves." @default.
- W1632660206 created "2016-06-24" @default.
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- W1632660206 date "1995-01-01" @default.
- W1632660206 modified "2023-09-27" @default.
- W1632660206 title "Upward Continuation to the Brillouin Level of the Romanian Gravity Map" @default.
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- W1632660206 doi "https://doi.org/10.1007/978-3-642-79721-7_26" @default.
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