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Abstract

Ocean bottom seismometer data were acquired by Mobil North Sea across the centre of the Faeróe-Shetland Basin to constrain its structural configuration where it is opaque to conventional seismic data due to pervasive basaltic intrusives.

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/content/papers/10.3997/2214-4609.201409219
1995-05-29
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409219
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