Research Portal
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Geoscience » Source Rock & Depositional Environment
Predictive Modeling of Sandstone Reservoir Distribution in the SW Scotian Basin
March 2018 – April 2020
The SW Scotian Basin is considered an under-explored passive margin sedimentary basin, however, it is also the most probable location to find oil on the Scotian Margin.
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.
Using Radar to Evaluate Seabird Abundance and Habitat Use at the Fundy Ocean Research Center for Energy Site near Parrsboro, Nova Scotia
April – September 2018
Shore-based seabird surveys conducted at the Fundy Ocean Research Center for Energy (FORCE) in Parrsboro, NS, determine abundance, habitat use and potential risk to seabirds at the site.
Measuring the Acoustic Detection Range of Large Whales from an Ocean Glider to Improve an Acoustic Whale Alert System for use by the Offshore Marine Industry in Atlantic Canada
April 2017 – January 2018
Researchers investigated a novel and in-development passive acoustic monitoring (PAM) system for use as a marine mammal detection technique. The work builds on a current research initiative between Dalhousie University and Woods Hole Oceanographic Institute (WHOI).
Finite Element Analysis to Assess Fish Mortality from Interactions with Tidal Turbine Blades
February – December 2017
The research project used finite element analysis (FEA) to simulate the impact of a tidal turbine blade on fish, and assess whether mortality of marine life can be expected in such an event.
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.