Observations of anomalous oceanic crust in the Canada Basin, Arctic Ocean
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Cited by (5)
Distribution of crustal types in Canada Basin, Arctic Ocean
2016, TectonophysicsCitation Excerpt :SB 1014 to the north of these sonobuoys and adjacent to Northwind Ridge has crustal velocities in the range of, 6.0–6.6 km/s overlying 7.4 km/s. SB 1015 slightly to the east records a 6.3 km/s layer overlying a 7.4 km/s refractor with an associated weak PmP arrival. This velocity range of above 7.4–7.5 km/s is compatible with an earlier result of Jackson et al. (1995) in the same area, suggesting that extremely thin, heterogeneous and possibly continental crust is a common character of this transitional zone in deep water near Northwind Ridge. Thirteen sonobuoys are classified as thinned continental crust and most have velocities of 5.5–6.6 km/s with no evidence of a higher velocity 7.2–7.6 km/s deep layer (Fig. 3a).
Chapter 50: Geology and tectonic development of the Amerasia and Canada Basins, Arctic Ocean
2011, Geological Society MemoirA new view on the origin of magmatism of the Franz Josef Land
2001, Izvestiya - Physics of the Solid EarthNew K-Ar ages for basalts from Franz Josef land
2001, Russian Journal of Earth Sciences
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