Research Portal
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Geoscience » Source Rock & Depositional Environment
Identifying and Constraining favourable paleoenvironments for the deposition of an Upper Jr SR using geochemical proxies (part of the PAGEO research program)
January 2021 – June 2023
This work will determine the paleoenvironmental conditions under which potential Upper Jurassic source rock intervals were deposited in offshore Nova Scotia.
Geoscience » Source Rock & Depositional Environment
Application of a source-to-sink sediment model to a petroleum systems analysis from field studies and numerical modeling (part of the PAGEO research program)
January 2021 – March 2023
This project will test the application of a source to sink analysis to the prediction of petroleum system elements in the Scotia Basin.
Review of Nova Scotia Power Transmission System Interconnection Requirements
April – May 2021
Power Advisory was engaged by OERA on behalf of the Nova Scotia Department of Energy & Mines to review the recently released Nova Scotia Power Transmission System Interconnection Requirements (TSIR) and identify any gaps between recommendations made by Power Advisory in their August 2020 repo
Net-Zero Future: A Feasibility Study of Hydrogen Production, Storage, Distribution and Use in The Maritimes - NL Extension
January – March 2021
This study investigated what role hydrogen can play in Newfoundland and Labrador’s future energy system.
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.