Abstract
Ocean Bottom Seismographs (OBS) are relatively commonly used in scientific lithospheric investigations in many parts of the world. On the Norwegian continental shelf several investigations of this kind have been performed during the last eight years as a result of the fruitful cooperation between the Institute of Solid Earth Physics, University of Bergen, the Laboratory for Ocean Bottom Seismology, Hokkaido University, the Laboratory for Earthquake Chemistry, Tokyo University, and Statoil.
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