SEAMSTRESS: DEPAS ocean-bottom seismometer operations on Vestnesa Ridge in 2020-2021

Cite as
Plaza-Faverola, Andreia; Domel, Przemyslaw; Bünz, Stefan; Schmidt-Aursch, Mechita; Schlindwein, Vera (2023): SEAMSTRESS: DEPAS ocean-bottom seismometer operations on Vestnesa Ridge in 2020-2021. GFZ Data Services. Dataset/Seismic Network. doi:10.14470/L4326155.
Identifier
10.14470/L4326155
FDSN network code
Y9
DataCite metadata
HTML | JSON | XML | INSPIRE | Local XML source file
Terms/rights
Creative Commons Attribution 4.0 International CC-BY-4.0 Request access
Creator(s)
orcid:0000-0001-7282-4277 Plaza-Faverola, Andreia a; orcid:0000-0001-6218-5432 Domel, Przemyslaw a; orcid:0000-0002-9215-7325 Bünz, Stefan b; orcid:0000-0002-2393-4514 Schmidt-Aursch, Mechita b; orcid:0000-0001-5570-2753 Schlindwein, Vera b
a UiT The Arctic University of Norway, b Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
  • (Abstract) “This ocean-bottom seismometer deployment is part of the SEAMSTRESS project examining tectonic stress effects on Arctic methane seepage. The project is led by PI Andreia Plaza-Faverola at the Centre for Arctic Gas Hydrates, University of Tromsö, Norway. A total of 10 ocean bottom seismometers (OBS) were deployed on Vestnesa Ridge, a sediment drift body just north Knipovich Ridge at its intersection with the Molloy Transform fault (cruise CAGE-20-5). The aim of the experiment was to look for stress release along faults that control seepage sites on Vestnesa Ridge. The network consisted of 8 Lobster type broadband OBS from the German Instrument Pool for Amphibian Seismology (DEPAS) and 2 3C geophones provided by the University of Tromsö. Instruments were free-fall deployed and spaced by about 10 km. They recorded continuously at 100 Hz for 11 months between August 2020 and July 2021.Short, intersecting refraction profiles were shot across all OBS stations, such that OBS positions at the seafloor could be determined within 10 m (cruise CAGE-21-3). Clock drift in this experiment was nonlinear and skew values were only obtained for 6 of the stations. Skew-corrected station VSN01 served as reference station to obtain the clock drift of all other stations using noise cross-correlation and subsequently correct also for the thus determined nonlinearity of time drift. Waveform data are available from the GEOFON data centre, under network code Y9.
Title
SEAMSTRESS: DEPAS ocean-bottom seismometer operations on Vestnesa Ridge in 2020-2021
Publisher
GFZ Data Services
Publication Year
2023
Dataset / Seismic Network
Dates
  1. Collected 2020-01-01
  2. Accepted 2023-05-01
  3. Created 2023-05-22
  4. Available 2025-07-01
Place(s)
  1. Vestnesa Ridge
Contributor(s)
  • Hosting institution: Deutsches GeoForschungsZentrum GFZ
  • Data manager: GEOFON Data Centre
  • Project leader: Alfred Wegener Institute (AWI), Bremerhaven, Germany
Subjects
Funding Reference(s)
  1. Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Language
en
Sizes
  1. 398GB
Reference(s)
FDSN network code
Y9
Network dates
2020–2021
Data time range
2020–2021
Station Count
8
Seismic metadata
fdsnws-station

To retrieve waveform data and metadata (including instrument responses) for this and other seismic networks, see here. Network (data set) values are taken from DataCite XML with Metadata Properties version 4.4. Contact us if you are the PI and wish to make changes. Old-style network page for this network here.

Station List for Network Code Y9

Code
Station description
Begin
End
Loc
Channels
Flags
VSN01
1st site
2020-08-22
2021-07-13
--
HDH HH1 HH2 HHZ
VSN03
3rd site
2020-08-23
2021-07-13
--
HDH HH1 HH2 HHZ
VSN04
4th site
2020-08-22
2021-07-15
--
HDH HH1 HH2 HHZ
VSN05
5th site
2020-08-22
2021-07-12
--
HDH HH1 HH2 HHZ
VSN06
6th site
2020-08-23
2021-07-13
--
HDH HH1 HH2 HHZ
VSN07
7th site
2020-08-23
2021-07-14
--
HDH HH1 HH2 HHZ
VSN08
8th site
2020-08-23
2021-07-13
--
HDH HH1 HH2 HHZ
VSN09
9th site
2020-08-23
2020-11-24
--
HDH HH1 HH2 HHZ