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TECHNICAL ARTICLES
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Published in issue No 106, October 2002 of The Hydrographic Journal
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DETAILED
BATHYMETRIC MAPPING AND SIDE SCAN SURVEYS IN THE INVESTIGATION OF COLD FLUID
VENT SITES AND ASSOCIATED GAS HYDRATE OCCURRENCES
Examples using mobile swath bathymetry and deep tow side scan
Jens Greinert PhD (Post Doctoral Fellow)
Wilhelm Weinrebe PhD (Head of the GEOMAR Data-Processing Centre)
GEOMAR Research Centre for Marine Gesciences, Kiel, Germany
Peter Gimpel PhD (Director Survey Systems)
Jörg Brockhoff (Product Support Manager)
L3 Communications ELAC-Nautik GmbH, Kiel, Germany
Abstract
Investigations of meter-scaled fluid expulsion sites, as active cold vents or
surface-near gas hydrate occurrences typically are called, require a detailed
bathymetric knowledge in order to pre-classify potential areas of fluid
expulsion for direct seafloor observations as well as TV-guided sediment
sampling and lander deployments. Coupled with side scan sonar investigations
more detailed information about the distribution of cold vent sites and their
typical methane-derived carbonate cementation of the sediment can be determined.
Gas hydrates which have formed close to the seafloor, are related to fluid vent
sites, where extensive methane expulsion occurs. This occurrence as well as the
distribution of carbonates can be investigated by side scan sonar and sub-bottom
profiler surveys ‘calibrated’ with direct seafloor observations. This enables
estimates of the regional quantity of surface-near gas hydrate, vent-induced
carbonates and active cold vent sites.
GEOMAR has been investigating cold vents in the North and South American Pacific
Coast, the Sea of Okhotsk and the Baltic Sea to study the geological,
geotechnical and biological cycles since 1987. During the joint German-Russian
project, KOMEX, in the Sea of Okhotsk, GEOMAR used a prototype swath bathymetry
system which was towed at the water surface. Equipped with a 50kHz BOTTOMCHART
MKII, this system enabled detailed bathymetric mapping independent of the vessel
used. In the Derugin Basin of the Sea of Okhotsk, where up to 10m high barite
build-ups cover the seafloor, bathymetric data sets the background for sediment
and dredge sampling.
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