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The Aeromag 1992 project covered Lersletten area in central West Greenland, just south of the southern edge of Disko Bay and the small village Ikamiut.
The geology of the area is not known in great detail because of limited field work . The area is situated within the Nagssugtoqidian mobile belt of the Precambrian Laurentian shield. The rocks of the Nagssugtoqidian belt consist mainly of Archaean basement, gneisses and supracrustal sequences, which have been reworked during Proterozoic time. Volcanic and plutonic rocks of Proterozoic juvenile origin, as well as Proterozoic supracrustal metasediments are also described. The tectonic structure of the Nagssugtoqidian is characterised by strong ENE linear trends, at places developed into steep belts with very strong shearing and sinistral displacement.
Several massive to semi-massive sulphide horizons in supracrustal sequences are identified and have been classified as sedimentary stratiform deposits.
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