Displaying 1 – 1 of 1 resultsFilters
Geoscience » Source Rock & Depositional Environment
Mid Cretaceous Sand Supply to Offshore SW Nova Scotia: Tectonic Diversion of Labrador Rivers during Naskapi Member Deposition
September 2015 – September 2017
This study tests the hypothesis that tectonic diversion of Labrador rivers during the Aptian resulted in sand supply through the Bay of Fundy to the Shelburne sub-basin, allowing shales to accumulate farther east in the Scotian Basin.