This study is a combined effort resulting from two cruises (SVAIS, of the BIO Hespérides and EGLACOM of the R/V OGS-Explora) within the International Polar Year (IPY) Activity 367 NICESTREAMS to resolve with the highest possible resolution the mechanisms of spatial and temporal changes in marine sedimentation on the Storfjorden and Kveithola Troughs Mouth Fans (TMFs) on the northwestern Barents Sea continental margin, from the Last Glacial Maximum to present. We used a combined geophysical, sedimentological and cronobiostratigrafic approach of the sedimentary sequence. Data analysis suggests strong across- and along-slope variability of the depositional system especially during the early phase of deglaciation
The north-western continental margin of the Barents Sea represents the only gateway for deep-water m...
Sediments on high Arctic shelves result from modern processes and the effect of former glaciations. ...
Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figuresMultibeam-...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
AbstractThe depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the no...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
The post Last Glacial Maximum depositional history of the Storfjorden and Kveithola trough-mouth fan...
European Geosciences Union General Assembly 2016 (EGU2016), 17-22 April 2016, Vienna, Austria.-- 1 p...
The development of two Arctic Trough Mouth Fans (TMFs), the Storfjorden and Kveithola TMFs, is inves...
© 2016 M. Pau & Ø. Hammer.A lithological and foraminiferal study of newly acquired sediment cores ou...
This thesis presents new results from marine geological and geophysical studies based on sediment gr...
A lithological and foraminiferal study of newly acquired sediment cores outside the Ingøydjupet (Ing...
The Bjørnøya Fan is located at the SW Barents Sea continental margin and consists of a succession of...
The Arctic Ocean is one of the most climatically vulnerable areas on the planet, being a crossway of...
The north-western continental margin of the Barents Sea represents the only gateway for deep-water m...
Sediments on high Arctic shelves result from modern processes and the effect of former glaciations. ...
Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figuresMultibeam-...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
AbstractThe depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the no...
The depositional history of the Storfjorden and Kveithola trough-mouth fans (TMFs) in the northweste...
The post Last Glacial Maximum depositional history of the Storfjorden and Kveithola trough-mouth fan...
European Geosciences Union General Assembly 2016 (EGU2016), 17-22 April 2016, Vienna, Austria.-- 1 p...
The development of two Arctic Trough Mouth Fans (TMFs), the Storfjorden and Kveithola TMFs, is inves...
© 2016 M. Pau & Ø. Hammer.A lithological and foraminiferal study of newly acquired sediment cores ou...
This thesis presents new results from marine geological and geophysical studies based on sediment gr...
A lithological and foraminiferal study of newly acquired sediment cores outside the Ingøydjupet (Ing...
The Bjørnøya Fan is located at the SW Barents Sea continental margin and consists of a succession of...
The Arctic Ocean is one of the most climatically vulnerable areas on the planet, being a crossway of...
The north-western continental margin of the Barents Sea represents the only gateway for deep-water m...
Sediments on high Arctic shelves result from modern processes and the effect of former glaciations. ...
Atlas of Submarine Glacial Landforms: Modern, Quaternary and Ancient.-- 2 pages, 1 figuresMultibeam-...