Abstract
Except for greater thickness and more pronounced lateral variations the Icelandic crust is very similar to the crust beneath the Reykjanes Ridge. Layer 3 can be traced without interruption from the 10 m.y. old oceanic crust on the southeastern flank of the ridge through Iceland. It exists also beneath the eastern neo- volcanic zone which is supposed to be the present spreading axis. Wide-angle reflection surveys across the active volcanic zones and the adjacent plateau basalts have given a detailed picture of the crust. The cross sections bear a certain resemblance to the crustal structure deduced from geological observations in Eastern Iceland. The dip of refractors and reflectors toward the axial zone and the absence of reflecting horizons below 8 km depth in the central part of the zone, support the predictions of models of crustal accretion mechanism. The episode of crustal rifting in the NE Iceland axial zone, which started in 1975 and still continues, has demonstrated how intimately the rifting is related to episodic magmatic processes at central volcanoes.
The subcrustal structure below Iceland is fundamentally different from the one below the southeastern flank of the Reykjanes Ridge. The Icelandic crust is underlain by low P-wave velocity (7.0 to 7.6 km/s) material down to depths greater than 50 km which is interpreted as mantle material in the state of partial fusion. This anomalous mantle seems to form a diapiric updoming of the astenosphere much broader than is likely beneath mid-ocean ridges proper. Magnetotelluric soundings indicate a low resistivity layer at the base of the crust. The depth to this layer is about 10 km beneath the axial rift zone but increases to about 17 km below the Tertiary basalts east and west. S-waves generally propagate in the crust beneath the axial rift zone to 10 km depth. At greater depth high P- to S-velocity ratio and attenuation of S-waves support the magneto- telluric evidence for partially molten basalt at the base of the crust, not only under the axial rift zone, but under the whole of Iceland.
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Bjornsson, S. (1983). Crust and Upper Mantle Beneath Iceland. In: Bott, M.H.P., Saxov, S., Talwani, M., Thiede, J. (eds) Structure and Development of the Greenland-Scotland Ridge. Nato Conference Series, vol 8. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-3485-9_3
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