Research Portal
Displaying 1 – 10 of 12 results
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
Scotian Shelf Oils Geochemistry
December 2019 – December 2020
Twenty-five significant hydrocarbon discoveries have been made on the Scotian Shelf in shallow water. Additionally, staining is observed in many wells and over a large geographical area.
Geoscience » Source Rock & Depositional Environment
Aspy Well Geochemistry
December 2019 – September 2020
This project determines if indications of migrated hydrocarbons or potential source rocks were encountered during the 2018 drilling of BP’s deep-water well Aspy D-11 well.
Geoscience » Source Rock & Depositional Environment
Seismic Reconstruction and Petroleum Systems Modeling of the Nova Scotia-Morocco Conjugate Margin
April – December 2019
Seismic Reconstruction
The Seismic Reconstruction project is a stand-alone element of the Conjugate Margin Program undertaken by the consulting firm Beicip Franlab. A number of subprojects and data streams are inputs to this project.
Geoscience » Source Rock & Depositional Environment
2018 Nova Scotia-Morocco Conjugate Geochemistry Project
May 2017 – June 2019
The objective of this project is to examine geochemical data from offshore and onshore Morocco to determine the presence and characteristics of effective Jurassic oil-prone source rocks.
Geoscience » Source Rock & Depositional Environment
Attenuation of Petroleum Generation Characteristics by the Sulfurization of Organic Matter in Westphaflan Carboniferous Lacustrine Source Rocks (A Geochemical Study of Potential Marine Incursions)
October 2017 – May 2019
This project creates geochemical diagnostic tools that can be applied to potential source rocks of differing ages in the Maritimes Basin. These tools help build a more accurate interpretation of the evolution of the basin.