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A 3D model (BARENTS3D) for the seismic velocity and density structure of the crust and upper mantle in the greater Barents Sea Region has been developed by a Norwegian-US team as a composite of two separate models, one for the crust (BARENTS50) and one for the upper mantle (BARMOD).
A. Škegro. Zbornik radova sa znanstvenog skupa "Duvanjski kraj kroz stoljeća", page 79-113. Tomislavgrad ; Zagreb, Naša ognjišta ; Hrvatski institut za povijest, (2000)