Research Portal
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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.
Valuation Method for Electric Ancillary Services
May – September 2020
The objective of this project is to define a new, enhanced power purchase agreement (PPA) for use by NSPI or an independent procurement administrator when contracting with Independent (e.g., renewable) Power Producers (IPPs).
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.
FORCE Site Marine Operations – Lessons Learned
November 2017 – April 2018
In recent years, marine operators have completed dozens of operations in the Minas Passage, from research surveys to instrument deployment, to the installation of electrical infrastructure to turbine deployment.
Nova Scotia Energy Sector – Targeted Export Market Analysis
February – October 2017
As part of Nova Scotia Department of Energy and Mines’ (NSDEM) mandate to investigate economic opportunities for Nova Scotia technology developers and supply chain service providers, a global energy market analysis was commissioned.
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.