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Crustal structure of the NE Rockall Trough from wide-angle seismic data modeling.

Klingelhöfer, F. and Edwards, R. A. and Hobbs, R. W. and England, R. W. (2005) 'Crustal structure of the NE Rockall Trough from wide-angle seismic data modeling.', Journal of geophysical research : solid earth., 110 (B11). B11105.

Abstract

Two wide-angle seismic lines located in the northern Rockall Trough were acquired in May 2000. One line (line E) crosses the trough from the continental shelf off Lewis to normal oceanic crust west of Lousy Bank in NW-SE direction. The other line (line D) intersects with line E, crosses the Wyville-Thomson Ridge in a SW-NE direction and ends in the Faeroe-Shetland Basin. Sonobuoy data and expanding spread profiles acquired in the same area have been remodeled. Analysis of the seismic data using travel times and amplitudes reveals an up to 5 km thick sedimentary basin including an up to 1.5 km thick basaltic layer which is present in most of the trough. Further conclusions of this study are that the Rockall Trough is underlain by highly stretched continental crust of ∼13 km thickness. The crust thickens to ∼24 km beneath Lousy Bank, which is interpreted to be of continental nature. Beneath the Hebrides continental shelf a three-layer continental crust of 26 km is modeled. An up to 12 km thick high-velocity layer is observed underneath the ocean-continent boundary and is interpreted as magmatic underplating resulting from excess volcanism during rifting. No evidence for an underplate layer could be distinguished beneath the trough area. Modeling of the structure of the Wyville-Thomson Ridge revealed no existing igneous core of the ridge confirming existing theories, that it is a compressional structure.

Item Type:Article
Keywords:Rockall Trough, Wide-angle seismics, Crustal structure.
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Status:Peer-reviewed
Publisher Web site:http://dx.doi.org/10.1029/2005JB003763
Publisher statement:Klingelhöfer, F., Edwards, R. A. , Hobbs, R. W. and England, R. W., (2005), Crustal structure of the NE Rockall Trough from wide-angle seismic data modeling, Journal of Geophysical Research: Solid Earth (1978–2012), 110(B11), B11105, 10.1029/2005JB003763 (DOI). To view the published open abstract, go to http://dx.doi.org and enter the DOI.
Date accepted:No date available
Date deposited:17 August 2015
Date of first online publication:November 2005
Date first made open access:No date available

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