Crustal structure of the Faeroe--Shetland Channel

• Published in: Geophysical Journal International
• Main Authors: Bott, Martin H. P., Smith, Peter J.
• Format: Text
• Language: English
• Published: Oxford University Press 1984
• Subjects: Articles; Rockall Trough; North Atlantic
• Online Access: http://gji.oxfordjournals.org/cgi/content/short/76/2/383; https://doi.org/10.1111/j.1365-246X.1984.tb05052.x

The deep structure of the Faeroe—Shetland Channel has been investigated as part of the North Atlantic Seismic Project. Shot lines were fired along and across the axis of the Channel, with recording stations both at sea and on adjacent land areas. At 61°N, 1.7 km of Tertiary sediments overlies a 3.9–4.5 km s-1 basement interpreted as the top of early Tertiary volcanics. A main 6.0–6.6 km s-1 crustal refractor interpreted as old oceanic crust occurs at about 9 km depth. The Moho (8.0 ° 0.2 km s-1) is at about 15–17 km depth. There is evidence that P n may be anisotropic beneath the Faeroe—Shetland Channel. Arrivals recorded at land stations show characteristics best explained by scattering at an intervening boundary which may be the continent—ocean crustal contact or the edge of the volcanics. The Moho delay times at the shot points, determined by time-term analysis, show considerable variation along the axis of the Channel. They correlate with the basement topography, and the greatest delays occur over the buried extension of the Faeroe Ridge at about 60° 15′N, where they are nearly 1 s more than the delays at 61°N after correction for the sediments. The large delays are attributed to thickening of the early Tertiary volcanic layer with isostatic downsagging of the underlying crust and uppermost mantle in response to the load, rather than to thickening of the main crustal layer. The new evidence is consistent with deeply buried oceanic crust beneath the Faeroe—Shetland Channel, forming a northern extension of Rockall Trough. The seabed morphology has been grossly modified by the thick and laterally variable pile of early Tertiary volcanic rocks which swamped the region, accounting for the anomalous shallow bathymetry, the transverse ridges and the present narrowness of the Channel.