about
Boundary condition of grounding lines prior to collapse, Larsen-B Ice Shelf, Antarctica.Interplay of grounding-line dynamics and sub-shelf melting during retreat of the Bjørnøyrenna Ice Stream.The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0Author Correction: Interplay of grounding-line dynamics and sub-shelf melting during retreat of the Bjørnøyrenna Ice StreamThe International Bathymetric Chart of the Southern Ocean (IBCSO) Version 1.0-A new bathymetric compilation covering circum-Antarctic watersMiocene reversal of bottom water flow along the Pacific Margin of the Antarctic Peninsula: Stratigraphic evidence from a contourite sedimentary tailVariability in Cenozoic sedimentation along the continental rise of the Bellingshausen Sea, West AntarcticaMiocene changes in bottom current regime recorded in continental rise sediments on the Pacific margin of the Antarctic PeninsulaOnset and growth of Trough-Mouth Fans on the North-Western Barents Sea margin – implications for the evolution of the Barents Sea/Svalbard Ice SheetThe carbonate mass transport deposits of the Paleogene Friuli Basin (Italy/Slovenia): Internal anatomy and inferred genetic processesPostglacial sedimentary processes on the Storfjorden and Kveithola trough mouth fans: Significance of extreme glacimarine sedimentationA Holocene paleosecular variation record from the northwestern Barents Sea continental marginOne Million Years of Climatic Generated Landslide Events on the Northwestern Barents Sea Continental MarginRecent Submarine Landslides on the Continental Slope of Storfjorden and Kveithola Trough-Mouth Fans (North West Barents Sea)Deglaciation of the western margin of the Barents Sea Ice Sheet — A swath bathymetric and sub-bottom seismic study from the Kveithola TroughSeabed morphology and shallow sedimentary structure of the Storfjorden and Kveithola trough-mouth fans (North West Barents Sea)Estimation of biogenic silica contents in marine sediments using seismic and well log data: Sediment Drift 7, AntarcticaChapter 1 Contourite ResearchLate Pliocene margin development and mega debris flow deposits on the Antarctic continental margins: Evidence of the onset of the modern Antarctic Ice Sheet?PrefaceReferencesThe present and past bottom-current flow regime around the sediment drifts on the continental rise west of the Antarctic PeninsulaInteraction of processes and importance of contourites: insights from the detailed morphology of sediment Drift 7, AntarcticaMargin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma: COMMENT AND REPLY: REPLYLate Pliocene Mega Debris Flow Deposit and Related Fluid Escapes Identified on the Antarctic Peninsula Continental Margin by Seismic Reflection Data AnalysisMargin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 MaRelationship between continental rise development and palaeo-ice sheet dynamics, Northern Antarctic Peninsula Pacific marginSubglacial morphology and glacial evolution of the Palmer deep outlet system, Antarctic PeninsulaEffects of biogenic silica on sediment compaction and slope stability on the Pacific margin of the Antarctic PeninsulaWater masses and bottom boundary layer dynamics above a sediment drift of the Antarctic Peninsula Pacific MarginErratum to: ‘Mid-late glacimarine sedimentary processes of a high-latitude, deep-sea sediment drift (Antarctic Peninsula Pacific margin)’Q57868822Mid-late Pleistocene glacimarine sedimentary processes of a high-latitude, deep-sea sediment drift (Antarctic Peninsula Pacific margin)Sediment drifts and deep-sea channel systems, Antarctic Peninsula Pacific MarginSeismic stratigraphy of Palmer Deep: a fault-bounded late Quaternary sediment trap on the inner continental shelf, Antarctic Peninsula Pacific marginGiant sediment drifts on the continental rise west of the Antarctic PeninsulaHigh-resolution sequence stratigraphy of clastic shelves IV: High-latitude settingsQ57874648Contourite depositional system on the Argentine Slope: An exceptional record of the influence of Antarctic water massesDeep-water Circulation: Processes & Products (16–18 June 2010, Baiona): introduction and future challenges
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