Abstract

An airborne radiometric survey was initiated in central West Greenland in 1975 folIowing completion of the aeroradiometric work in East Greenland (Nielsen, 1972; Nielsen & Larsen, 1974). During, 1975 the region between Søndre Strømfjord and Jakobshavn Isfjord was covered, an area of c. 58 000 km2. The programme was carried out as a collaboration between GGU and the Danish Atomic Energy Commission's Research Establishment, Risø. GGU and Risø each supplied three participants. The aircraft, a Britten-Norman Islander, were chartered through Greenlandair Charter AIS. Aeromagnetic measurements were carried out simultaneously (Thorning, this report). Field operations were carried out from Søndre Strømfjord Air Base. It is planned to continue this radiometric survey duiing the next few years, including follow-up fieldwork on the ground.

Highlights

  • GGU and Risø ~ach supplied three participants

  • All major geological formations were investigated, except for areas covered by Quaternary and younger deposits. which make up about 20 per cent of the area

  • Rock units mention·ed below follow the divisions made on the geologicalmap SøndreBtrømfjord-NOgssuaq, scale 1:500 000 (GGU, 1971)

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Summary

Karsten Secher

An airborne radiometric survey was initiated in central WestGreenlandin 1975 folIowing completion of the aeroradiometric work in East Greenland 1975 the region between Søndre Strømfjord and Jakobshavn Isfjord was covered, an area of c. 58 000 km2 The programme was carried out as a collaboration between GGU and the Danish Atomic Energy Commission's Research Establishment, Risø. GGU and Risø ~ach supplied three participants. The aircraft, a Britten-Norman Islander, were chartered through Greenlandair Charter AIS. Aeromagnetic'measurements were carried out simultaneously (Thorning, this report). It isplanned to continue this radiometric survey duiing the few years, inc1uding follow-up fieldwork on the grouild

Equipment and methods
Remarks an the radiaactivity
Ikertoq gneiss complex
Egedesminde gneiss complex
Findings
Concluding remarks
Full Text
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