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USGS CMG S-96-94-WG Metadata

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Metadata
ID S-96-94-WG
Also Known As SO96
Abstract Chief Scientists: Roland Von Huene, Ernst Flueh. Geochemical and Geophysical data (bathymetry, magnetics, bottomseismometer) of field activity S-96-94-WG in Western Gulf of Alaska from 07/28/1994 to 08/29/1994
Project/Theme Seisvent
Chief Scientist Roland Von Huene
Ernst Flueh
Activity Type Geochemical and Geophysical
Platform F. S. Sonne
Area of Operation
Western Gulf of Alaska
Location map S-96-94-WG location map of where navigation equipment operated
Bounding Coordinates 61.75000
-156.00000    -144.25000
54.00000
Dates 07/28/1994 (JD 209) to 08/29/1994 (JD 241)
Analog Materials No analog holdings.
Index map

S-96-94-WG map of where navigation equipment operated

Crew
Roland Von Huene Chief Scientist, USGS Western Region
Ernst Flueh Chief Scientist, GEOMAR
Equipment Used
bathymetry
magnetics
bottomseismometer
Purpose
Active seeping of fluids, including greenshouse gasses, from the accretionary wedge might influence global climate. Fluids also strongly influence the mechanics of faults in the wedge.
Summary
Used USGS and hydrosweep data to locate potential site where fluids seep from the accretionary wedge. The lower continental slope off Kodiak Island was surveyed using Hydrosweep.
Notes
USGS contact: Mike Fisher
(from 9/2/94 USGS Bulletin) During July the German research ship Sonne
conducted geochemical and geophysical research in the Gulf of Alaska. Chief
scientists Roland Von Huene and Ernst Flueh of GEOMAR in Germany were
interested in measuring the flux of greenhouse gasses from the accretionary
wedge near the Aleutian Trench. Multichannel seismic and Hydrosweep
bathymetric data provided initial clues to locate potential fluid seeps, and
the geochemists investigated likely sites using a video-camera sled. Although
we found no obvious seeps, ever optimistic scientists hoped that the following
cruise would identify additional sites for detailed analysis. Another research
goal was to collect detailed seismic-velocity information from accreted rocks
near the trench. From these data, geophysicists hoped to calculate gradients
in the degree of compaction of accreted sediment as well as the volume of
fluid expelled. The seismic source was two monstrous (2000 cu. in. each) air
guns. Ten OBSs were deployed repeatedly with great success in this endeavor.
Unfortunately, foul weather foiled our attempt to measure the seismic velocity
of highly reflective rocks that form the middle and lower crust of the
accretionary complex near lower Cook Inlet. The highlight of the cruise came
with our realization that enigmatic features in USGS and Hydrosweep data
revealed collision scars that resulted from subduction of seamounts and
collision of the Yakutat terrane. Mike Fisher
Got Help? For S-96-94-WG, we would appreciate any information on -- analog materials, contract, days at sea, dive count, funding, information specialist, information to be derived, kms of navigation, national plan, NGDC Info, organization, owner, ports, project number, publications, scanned materials, seismic description, station count, station description, submersible, tabulated info.

 

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