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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 » 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 » 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 » 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 » Georges Bank Research & Data

Science and Socio-economic Review of the Georges Bank Prohibition Area 2020-2021

June – December 2021

Georges Bank is a large submarine platform located at the edge of the Atlantic continental shelf between Cape Cod and Nova Scotia. The Georges Bank Prohibition Area covers a significant portion of Georges Bank and is located on the Canadian side of the Canada-United States maritime boundary.

Geoscience » Source Rock & Depositional Environment

Microbial Genomics for De-Risking Offshore Oil and Gas Exploration in Nova Scotia

April 2016 – March 2021

The purpose of this $6.5M project is to develop, validate and deploy different genomics-based bioassay tools for offshore prospecting on the Scotian Slope.

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

Predictive Modelling of Sandstone Reservoir Quality in the Scotian Basin

May 2016 – December 2018

This project uses existing knowledge of inferred drainage basin areas and paleoclimate to model multiple river inputs to the Scotian Basin. The modelled sedimentary succession is compared with actual sediment thicknesses in the basin.

Geoscience » Spill Preparedness

Advanced Coastal Mapping to Support Hydrodynamic Modelling

April 2016 – June 2018

Nova Scotia’s Atlantic coast exhibits a variety of shorelines that may be vulnerable to contamination in the event of an offshore oil spill. In turn, variable currents, changing water levels, shoals, and exposed seaside conditions make effective spill response difficult for tidal inlets.

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.