Scheduled Cruises in 2003
Summary of a recent cruise on margins research (RU.031)
Norwegian margin (Leg 1)
Professor Logachev
Copenhagen, Denmark. 14 Jul 2003
Tromsø, Norway. 30 Jul 2003
To study several diapir
fields within the Vøring Plateau area of the Norwegian margin. They are
of different sizes and surface expressions and their origin is unknown.
As a continuation of earlier work, seismic and acoustic studies and
bottom sampling are planned on the Vivian and Vigrid Fields, located on
the Vøring Marginal High and Vøring Basin, respectively, to study the
diapirs' morphology, the structural control of their location and
distribution and the possible relationship to fluid-venting through the
seafloor.
The Traenadjupet Slide off the
northern part of Norway covers an area of about 12000 km2.
It originated on the continental slope and has a well-defined
termination on the lower continental rise. The distal part of the slide
will be studied to elucidate the sediment failure processes and their
ages. The sedimentary processes, stratigraphy and sediment rate/flux of
the deep-sea fan deposited in the Lofoten Basin at the mouth of the
Lofoten Basin Channel are also planned to be studied with a
high-resolution side-scan sonar, seismics and bottom sampling.
The Andøya Slide is a large-scale
slide on the northern Norwegian continental margin. It covers an area
of about 9700 km2. No dated cores are available from the
slide-affected area. The cruise will use high-resolution side-scan
sonar, seismics and coring to date the base of the sediments overlying
the slide sediments and thus getting the latest age for the slide
event. Also, the Andøya Slide is located close to a large canyon, the
Andøya Canyon. Side-scan sonar data is necessary in order to identify
the origin of the sediments to be cored and make sure that these
originate from the Andøya Slide.
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