Seafloor Structure in the North Atlantic Region between the Kolbeinsey Ridge and the Jan Mayen Microcontinent

— Deep seismic sounding, continuous seismic profiling, and bathymetric data are used to discuss the structure of the Iceland Plateau and adjacent areas of the Norway–Greenland region. We tentatively suggest the existence of regional nearly NS-trending tectonic discontinuities; these are normal fault...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Izvestiya. Atmospheric and oceanic physics 2018-12, Vol.54 (11), p.1546-1558
Hauptverfasser:	Usenko, S. V., Boiko, A. N., Prokhorova, T. V.
Format:	Artikel
Sprache:	eng
Schlagworte:	Bathymetric data Climatology Depth profiling Dikes Earth and Environmental Science Earth Sciences Embankments Fault zones Geological faults Geophysics/Geodesy Heat flow Heat transmission Magnetic anomalies Mantle plumes Ocean floor Plateaus Tectonics
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Schreiben Sie den ersten Kommentar!