Results 251 to 260 of about 208,933 (390)
Basal conditions that facilitate fast ice flow are still poorly understood and their parameterization in ice‐flow models results in high uncertainties in ice‐flow and consequent sea‐level rise projections. Direct observations of basal conditions beneath modern ice streams are limited due to the inaccessibility of the bed.
Rebecca Schlegel+5 more
wiley +1 more source
Feeding postures as indicators of mutable collagenous tissue in extinct echinoderms. [PDF]
Waters JA, Jan Bohatý, Macurda DB.
europepmc +1 more source
Stratigraphy and structure in Mount Hulcross-commotion Creek map-area, British Columbia
R T D Wickenden, George Shaw
openalex +1 more source
Automated delineation and morphometry of unclassified subglacial bedforms
We present an automated tool for mapping and analysing subglacial bedforms using volumetric obscurance, without classification. Tested on ArcticDEM data, the method produces bedform outlines with 75% correspondence compared to manually digitized maps.
Sofyane Hesni+5 more
wiley +1 more source
High resolution 3-D seismic and sequence stratigraphy for reservoir prediction in 'Stephi' field, offshore Niger Delta, Nigeria. [PDF]
Oluwadare OA+3 more
europepmc +1 more source
Stratigraphy and Geological Structure of the Eastern Area of Shima Peninsula
Nobuo Yamagiwa
openalex +2 more sources
Relative sea‐level trends in southern Norway during the last millennium
Relative sea level in southern Norway has been falling since c. 7000 cal. yr BP, but modern tide gauge data show rising relative sea level since at least 1960 CE. In this study, peat cores from a shallow coastal basin were analysed, using a multiproxy approach, to reconstruct relative sea level trends over the last millennium and to identify the onset ...
Max Holthuis+10 more
wiley +1 more source
Enhancing in search of Milankovitch cycles from stratigraphic record using convex optimization algorithm. [PDF]
Alam S+3 more
europepmc +1 more source
We have mapped a 60 km long, 30 km wide, 120 m deep buried glacially eroded trough on the North Sea Plateau, west of the Norwegian Channel (59°N, 3°E). The trough was carved out by an ice stream that flowed out from western Norway and crossed the Norwegian Channel in a southwestern direction during the penultimate or Saalian glaciation.
Dag Ottesen+4 more
wiley +1 more source