1 National Space Institute, Technical University of Denmark2 Geomagnetism, National Space Institute, Technical University of Denmark3 J. W. Goethe-University
Despite a well-mapped, interesting surface geology, deep sounding geophysical studies like seismics or magnetotellurics have been used very rarely in Greenland. The aim of this article is to present the preliminary results of a magnetotelluric study performed in the area of Kangerlussuaq, West Greenland. The estimated transfer functions will be used in the future for 2-D and 3-D modelling of subsurface resistivity structures, the inuence of the electrically conductive ocean, as well as the source geometry in the auroral oval.
Proceedings of the 24th Schmucker-weidelt-kolloquium Neustadt an Der Weinstraße, 2011, p. 142-145