POSEIDON POS458

Area:
Eastern Atlantic; Galizien
Time:
25.08.2013 - 15.09.2013
Institution:
GEOMAR
Chief scientist:
Dirk Klaeschen

During the opening of the Atlantic Ocean Portugal and Spain got separated from Newfoundland. Such a continental breakup is preceded by stretching and thinning of the continental crust and lithosphere. At some continental margins, such as the margin west of Galicia (northern Spain), late stages of extension are dominated by motion on faults with very low angles of dip underlain by serpentinized peridotite, and thought to be upper mantle exhumed to the seafloor during rifting. This deformation, with rotated continental crustal blocks, is highly three-dimensional, but has yet to be imaged in three dimensions.

In June-July 2013, a three-dimensional seismic survey was conducted on the Galicia margin by project partners from USA, UK, and GEOMAR. The project involved the largest academic three-dimensional seismic survey completed to date while making 3-D images of the water column, and the upper 20 kilometers of the rocks under the seafloor. The survey was carried out by RV MARCUS G. LANGSETH, owned by the NSF and operated by the Lamont-Doherty Earth Observatory (USA) and covered a rectangular area of 86 by 22 kilometers.

In May-June, before the Langseth sailed from Vigo (Spain), the German Research Vessel POSEIDON Cruise P453 left Vigo with scientists from GEOMAR and the United Kingdom and deployed 78 ocean-bottom seismometers and collected contemporary hydrographic data in a grid on the same area of ocean floor that the Rice University (USA) team on the LANGSETH were surveying. The ocean-bottom seismometers recorded all airgun shots of the 3d-seismic system and gave additional information about the rocks of the continental crust and upper mantle. The aim is to use the resulting unique dataset to enhance the understanding of large-scale lithospheric extension as well as to provide a possible constraint for seismic oceanography analysis.

During the actual cruise P458 the 78 ocean-bottom seismometers will be recovered again. The instruments recorded on the seafloor in a depth of 5000m over 11 million airgun shot recordings during the last three months.