Late Cenozoic stratigraphy and environment in the Barents Sea

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Vorren, Tore O. ; Hald, Morten ; Lebesbye, Erland ; Vorren, Karl-Dag (1987)
  • Publisher: Co-Action Publishing
  • Journal: Polar Research (issn: 1751-8369, eissn: 1751-8369)
  • Related identifiers: doi: 10.3402/polar.v5i3.6895

Evaluation of the geology of the late Cenozoic Barents Sea is based upon several thousand km of seismic profiles. several hundred gravity cores and some ten 100 m deep corings taken by drilling vessels.
  • References (2)

    Fig. I . A tentative model of the deglaciation pattern and chronology of the Barents Sea. The model is based on several sources, e.g. E l v e r h ~ i & Solheim (1983).Vorren & Kristoffersen (1986). Mangerud et al. (1987). Vorren et al. (1988) and some unpublished data.

    The contour interval is 100m on the shelf and 200 m on the slope.

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