Abstract
A low frequency sound propagation experiment was conducted in the Western Barents Sea from a towed continuous sound source and air-dropped explosive sound sources to a hydrophone lying on the sea bed. Anomalies in the propagation results were traced to sub-bottom features, in particular to a region of basement outcrop. This paper will present data suggesting the influence of a particular salt diapir occurring within this basement outcrop region upon the low frequency sound propagation. The results suggest alternative interpretations for the mechanism of influence of the sea-bed upon the sound field.
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References
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© 1986 Plenum Press, New York
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Hug, E.H. (1986). A Propagation Anomaly Observed in the Barents Sea. In: Akal, T., Berkson, J.M. (eds) Ocean Seismo-Acoustics. NATO Conference Series, vol 16. Springer, Boston, MA. https://doi.org/10.1007/978-1-4613-2201-6_22
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DOI: https://doi.org/10.1007/978-1-4613-2201-6_22
Publisher Name: Springer, Boston, MA
Print ISBN: 978-1-4612-9293-7
Online ISBN: 978-1-4613-2201-6
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