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Nature of the Iceland Plateau and northeastern Iceland shelf, Northeast Atlantic

Subject Area Geophysics
Term since 2026
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 564747023
 
With this marine geophysical survey, we aim to reveal the distribution of oceanic versus continental crust between the Jan Mayen Microplate Complex and the Faroe continental plateau. Major open question is the fate and amount of continental material now dispersed in the Northeast Atlantic as a consequence of the rift migration from the Aegir Ridge to the Kolbeinsey Ridge. Currently, competing hypotheses denote the crustal composition of the Iceland Plateau as (i) thickened oceanic (mafic) crust, (ii) stretched continental crust and possibly exhumed mantle or (iii) oceanic rift migration by rift jumps with embedded continental fragments. We propose (i) a multi-channel seismic reflection grid over the Iceland Plateau to identify deformation phases, structures and tectonic domains, (ii) two seismic refraction profiles over the Iceland Plateau and the Iceland shelf to determine the crustal composition, and (iii) a high resolution magnetic mapping of the southern termination of the extinct Aegir mid-oceanic ridge to test the presence of a possible transform fault at the southern boundary of the Norway Basin. The combination of seismic reflection and refraction, both optimized to low frequencies to acquire data below basalts and to allow full waveform inversion of the data, magnetics and gravity shall enable us to get a significantly enhanced understanding of the complex opening processes of the central Northeast Atlantic.
DFG Programme Infrastructure Priority Programmes
International Connection Iceland
Co-Investigator Dr. Dieter Franke
Cooperation Partner Dr. Anett Blischke
 
 

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