Contourite drifts, channels and moats in the deep epeiric Late Cretaceous Chalk Sea of NW Europe

• Finn Surlyk ^[1]
  1. [1] University of Copenhagen

     University of Copenhagen

     Dinamarca

     
• Localización: Geotemas (Madrid), ISSN 1576-5172, Nº. 11, 2010 (Ejemplar dedicado a: Deep-Water Circulation: Processes & Products. International Congress. Baitona, Pontevedra, Spain. 16 & 17 June 2010), págs. 167-168
• Idioma: inglés
• Enlaces
  • Texto Completo Ejemplar
• Resumen

  • The Upper Cretaceous – Danian Chalk Group of NW Europe was in wide areas strongly influenced by contour-parallel bottom currents forming large drifts, moats and channels.