Preliminary Bouguer anomalies of western North Greenland

Abstract

During the summer af 1979 the Geodetic Institute, Copcnhagen, continued the North Greenland survey, which was initiated in 1978 (Forsberg, 1979). This comprised establishment of ground control points by help of Doppler instruments combined with barometric, triangulation and doppler-derived heights as vertical control. During 1979, as a minor part of the surveying programme, a regional gravity network was established for the area belween Hall Land and Nansen Land (fig. 66).