Imaging igneous intrusions in the lower crust on the Faroes and Hatton Bank margins using wide-angle Ocean Bottom Seismometer data.

Stacked seismic sections produced from wide-angle ocean bottom seismometers (OBS) show clear, strong P-wave reflections interpreted as igneous intrusions arriving from lower crustal and upper mantle depths on the Faroes margin. The lower-crustal reflectors are also seen on a coincident long- offset...

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Bibliographic Details
Main Authors: Lewis, O. J., White, R. S., Christie, P. A. F.
Format: Conference Object
Language:unknown
Published: 2009
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/1319/