Research Portal
Displaying 1 – 6 of 6 results
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.
In Situ Turbulence Replication and Measurement (InSTREAM)
October 2015 – January 2018
The In Situ Turbulence Replication and Measurement (InSTREAM) project was conceived to address some fundamental questions about the turbulence physics in tidal energy sites and laboratory tanks used to simulate these sites.
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.
Going with the Flow: Advancement of Drifting Platforms for use in Tidal Energy Site Assessment & Environmental Monitoring
April 2015 – August 2017
This research project aimed to apply a simple and low cost philosophy to ocean observation by developing an inexpensive low-profile surface drifter for use in initial assessment of potential tidal energy development opportunities. The project addressed limitations in the existing drifter design
Geoscience » Tectonics and Crustal Structure
Extensional Tectonics across the Northern Nova Scotia Margin from Ocean Bottom Seismic Data
May 2015 – April 2017
This project analyzes two wide-angle refraction/reflection ocean-bottom seismometer profiles recently collected offshore north-central Nova Scotia.
Turbulent Scale and Wake Modeling on a Horizontal Axis Turbine
January – April 2015
This project aimed to accurately simulate turbulent flow over a scaled horizontal axis tidal turbine to resolve turbulence in the near and far field regions.