English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Plus monthly

Global: Zendy Tools annual

Global: Zendy Tools monthly

Global: Zendy Free Plan

A database of interpreted geological cross-sections assembled from analogue high-resolution seismic-reflection profiles from Sable Island Bank has been compiled. A preliminary seismostratigraphy has enhanced understanding of the mid–late Pleistocene section. Numerous units and their bounding unconformities indicate a complex history of glaciogenic and sand-sheet deposition and associated sea-level fluctuations. A near-shelf-break ice-maximum position is interpreted for the Late Wisconsinan and inferred for earlier stades and/or glaciations. A late readvance sometime between 16 ka and 14 ka deposited a thick sand body over the transgressed bank, forming ancestral Sable Island. Modification and transport of sands accompanied a subsequent transgression. The database will provide the basis for compilation of a lithological and geotechnical zonation and a suite of maps depicting unit thickness and distribution, unconformities, and subsurface features, including geohazards, as well as large-scale (>1.5 m high) surficial bedforms. 2001-D19 E.L. King 1 CURRENT RESEARCH RECHERCHES EN COURS 2001 Article Article Titles Titres Purchase Information Information pour acheter

A glacial origin of Sable Island: ice and sea-level fluctuations from seismic stratigraphy on Sable Island Bank, Scotian Shelf, offshore Nova Scotia