Gas hydrate in the southern Barents Sea, indicated by a shallow seismic anomaly

K. Andreassen; K. Hogstad; K.A. Berteussen

doi:10.3997/1365-2397.1990012

ISSN: 0263-5046
E-ISSN: 1365-2397

Gas hydrate in the southern Barents Sea, indicated by a shallow seismic anomaly
By K. Andreassen, K. Hogstad and K.A. Berteussen
Source: First Break, Volume 8, Issue 6, Jun 1990,
DOI: https://doi.org/10.3997/1365-2397.1990012
- Published online: 01 Jun 1990

Abstract

A shallow seismic reflector of anomalous. high amplitude cuts through dipping layers of Late Palaeocene age in the southern Barents Sea. The seismic event is observed on a high-resolution, multi-channel seismic profile as well as on conventional deep seismic lines. The anomaly is situated at a depth of 525 m below sea-level and 180 m below sea-bottom (water depth is 345 rn).

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1990-06-01

2024-04-18

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Article Type: Research Article

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Gas hydrate in the southern Barents Sea, indicated by a shallow seismic anomaly

Abstract

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