Project BEAR ISLAND: DEPAS ocean-bottom seismometer operations in the Fram Strait in 2007-2008

DOI

BEAR ISLAND (The Dynamic Continental Margin Between the Mid-Atlantic-Ridge System (Mohns Ridge, Knipovich Ridge) and the Bear Island Region) is an interdisciplinary project exploring the stress conditions and sources, and the dynamics and deformation characteristics of the continental margin between the Mid-Atlantic Ridge and Bear Island from its top sedimentary cover to its imprint in the upper mantle. In this region the margin includes an extremely thick sedimentary wedge and steep slopes, with at least one major paleo-fracture zone cutting through the wedge. Recent studies in this area indicate very low seismic velocities in the lithosphere and the stress field undergoes an extensional-compressional transition. It is therefore of particular interest to understand the structural architecture, the stress and the dynamics of the whole region because of its natural hazard exposure and the processes involved in the formation of the margin and the opening of the North Atlantic.To achieve this, deep seismic sounding data, as well as records from temporary broadband installations, supplementary to data from existing seismic stations in the region were collected. A key element of the project was the operation of a long-term network of broadband ocean-bottom seismometera (OBS). Additionally, two new broadband seismometers and a small temporary seismic array with 13 sensors were operated. Active seismic refraction/reflection experiments were conducted along two profiles crossing the region and recorded with additional short period OBSs and land stations.Twelve broadband coean-bottom seismometer (OBS) from the German Instrument Pool of Amphibian Seismology (DEPAS) were deployed as part of this network with RV Horyzont II in September 2007. They were distributed on the Barents shelf, the slope and the deep sea near the Mid-Atlantic Ridge. Nine instruments could be recovered in August 2008 with RV Horyzont II. One instrument was fished before, one was destroyed during recovery and one got lost. Seven stations recorded data for the full deployment period; two stations have no skew value. Based on previous experiments, the accuracy of the positions is estimated to 500 m.

Identifier
DOI https://doi.org/10.1594/PANGAEA.972423
Related Identifier References https://doi.org/10.17815/jlsrf-3-165
Related Identifier References https://doi.org/10.1111/j.1365-246X.2010.04873.x
Related Identifier References https://doi.org/10.1029/2010JB007889
Related Identifier References https://doi.org/10.1007/s11001-012-9155-3
Related Identifier References https://doi.org/10.1007/s10950-017-9692-y
Related Identifier References https://doi.org/10.1016/j.jog.2018.01.013
Related Identifier References https://doi.org/10.21348/P.2011.0001
Related Identifier References https://doi.org/10.21348/P.2008.0001
Related Identifier References https://doi.org/10.1785/0220210018
Related Identifier References https://doi.org/10.31905/TYLLQY8T
Related Identifier References https://doi.org/10.14470/4P044426
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.972423
Provenance
Creator Schweitzer, Johannes; Schmidt-Aursch, Mechita ORCID logo; Krüger, Frank; Guterch, Aleksander
Publisher PANGAEA
Publication Year 2024
Funding Reference The Research Council of Norway https://doi.org/10.13039/501100005416 Crossref Funder ID 176069 https://prosjektbanken.forskningsradet.no/en/project/FORISS/176069 The Dynamic Continental Margin Between the Mid-Atlantic-Ridge System (Mohns Ridge, Knipovich Ridge) and the Bear Island Region
Rights Creative Commons Attribution 4.0 International; https://creativecommons.org/licenses/by/4.0/
OpenAccess true
Representation
Resource Type Dataset
Format text/tab-separated-values
Size 237 data points
Discipline Earth System Research
Spatial Coverage (6.139W, 72.850S, 15.851E, 75.544N); Fram Strait
Temporal Coverage Begin 2007-09-19T07:27:00Z
Temporal Coverage End 2008-08-19T10:40:00Z