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...
Main Authors: | , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2009
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Subjects: | |
Online Access: | http://eprints.esc.cam.ac.uk/1319/ |