Research Portal

Geoscience » Tectonics and Crustal Structure

Geologic Origin of Deep Crustal and Uppermost Mantle Structures at the Continent-Ocean Transition Offshore Nova Scotia from Modeling of Wide-Angle S-Wave Arrivals (part of the PAGEO research program)

January 2021 – June 2023

This work will produce S-wave velocity models for two of the existing refraction profiles from the Scotian margin. The objective is to better constrain the crustal origin of the continent-ocean transition (COT) using both the P and S-wave velocity models.

Geoscience » Tectonics and Crustal Structure

Prospectivity of the Shelburne Subbasin, Scotian Margin: An Integrated Multidisciplinary and Multiparameter Approach from Plate to Pore Scale (part of the PAGEO research program)

January 2021 – June 2023

This project will significantly increase our understanding of both the reservoir potential of Tertiary sequences within the Shelburne Subbasin, offshore Nova Scotia, and the crustal architecture underlying this critical region located at a proposed transition from a magma-rich to a magma-poor con

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.

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

Drones and Drifters – The Great Pumpkin Race

October 2016 – July 2017

This project tested and developed a new low-cost approach to collecting oceanographic measurements for use in tidal initial site assessments. The plan combines one of the oldest tools in oceanography, the drifter, with one of the newest, the drone.

Tidal Turbine Marine Life Interaction Study: Fish

May 2016 – May 2017

This study at Dalhousie University’s Aquatron test tank monitored the behaviour of striped bass in the presence of an active tidal turbine.  The research drew on expertise and experience from different parts of Canada and Europe over a one year project period.

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.

Use of Bottom-Mounted Hydro-Acoustic Sonar to Assess Fish Presence and Vertical Distribution at the FORCE In-Stream Tidal Turbine Test Site in Minas Passage

May 2016 – April 2017

To better understand fish use of the Fundy Ocean Research Center for Energy (FORCE) site and their potential for interaction with in-stream tidal devices, this study examined how fish density and vertical distribution varied with respect to environmental factors, in particular tidal stage and tim