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Ocean-bottom seismometers (OBS) are used offshore to explore architecture and structure of the earth's crust and mantle, e.g at passive continental margins, subduction zones oder mid-ocean ridges. The registration of earthquakes (seismology) or of artificial sound waves (seismic refraction) yields conclusions about the properties of the subsurface in different depths. |
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Contacts
Role | Name |
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Engineer in Charge | Henning Kirk |
Data Scientist | Mechita Schmidt-Aursch |
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