Research Portal
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Geoscience » Source Rock & Depositional Environment
Sequence stratigraphy, titania diagenesis and relationship to petroleum systems modeling
October 2018 – January 2021
This project examines different forms of titania (TiO2) minerals to confirm the relationship between late diagenetic titania (i.e., titania minerals transformed under the heat and pressure of sedimentary processes) and hydrocarbon migration and thus assess the use of titania polymorphs as “pathfi
Feasibility Study: Tidal Sector Service Barge/Drydock
April – November 2018
The study investigates the feasibility of developing a generic, shared-use, multi-function turbine transport deployment and retrieval barge/drydock for use by the Nova Scotia tidal energy sector.
Using Dry Ports to Support Nova Scotia’s Tidal Industry
March – June 2018
This study investigates two Nova Scotia “dry ports” and their potential in supporting the Bay of Fundy region’s emergent tidal energy industry. The term ‘dry port’ refers to a port where the harbour bottom is mainly exposed at low tide.
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.