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.
|Title of host publication||Proceedings of the 24th Schmucker-Weidelt-Kolloquium Neustadt an der Weinstraße|
|Place of Publication||Germany|
|Publisher||Deutsche Geophysikalische Gesellschaft|
|Publication status||Published - 2011|
|Event||24. Schmucker-Weidelt-Kolloquium - , Germany|
Duration: 19 Sep 2011 → 23 Sep 2011
|Period||19/09/2011 → 23/09/2011|