Research Portal
Displaying 1 – 6 of 6 results
Geoscience » Source Rock & Depositional Environment
Tracking Mesozoic Paleoclimate Events on the Nova Scotia Margin: Integrating Biostratigraphic Legacy Data with New Stable Carbon Isotope Analyses (part of the PAGEO research program)
November 2020 – November 2021
This study will obtain empirical evidence for climatic perturbations and regional changes in oceanic circulation patterns by (1) acquiring an extensive dataset of stable isotope measurements from key wells located in the area of interest, (2) integrating these measurements with existing quantitat
Geoscience » Source Rock & Depositional Environment
Analysis of Palaeoenvironment, Palaeoclimate and Palaeooceanographic Models to Predict Distribution of Source Rocks Offshore Nova Scotia (part of the PAGEO research program)
November 2020 – June 2021
The objective of this work is to predict the distribution of Tithonian and early Jurassic (Toarcian, Pliensbachian, Sinemurian, Hettangian) source rocks based on biogeographic principles derived from modern environments, and palaeoenvironmental interpretations derived from palaeogeographic mappin
Geoscience » Source Rock & Depositional Environment
Scotian Shelf Oils Geochemistry
December 2019 – December 2020
Twenty-five significant hydrocarbon discoveries have been made on the Scotian Shelf in shallow water. Additionally, staining is observed in many wells and over a large geographical area.
Geoscience » Source Rock & Depositional Environment
Aspy Well Geochemistry
December 2019 – September 2020
This project determines if indications of migrated hydrocarbons or potential source rocks were encountered during the 2018 drilling of BP’s deep-water well Aspy D-11 well.
Geoscience » Source Rock & Depositional Environment
Piston Coring Geochemistry Program
January 2015 – January 2020
Confirming the presence of hydrocarbons from an oil-prone Jurassic age source rock would encourage exploration in the deep water portion of Nova Scotia’s offshore.
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.