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Geoscience » Source Rock & Depositional Environment
Nova Scotia-Morocco Conjugate Biostratigraphy Project
September 2018 – June 2019
Biostratigraphy, the study of fossils to determine the age and depositional conditions of the sediments from which they are recovered, is a critical input to the seismic reconstruction of the Nova Scotia and Morocco margins. Detailed biostratigraphical analyses have been completed by an internat
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.