Research Portal
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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 » Tectonics and Crustal Structure
Paleogeographic Reconstruction and Source Rock De-Risking, Offshore Nova Scotia
February – November 2020
In this project GeoArctic modeled the tectonic evolution of the northern Central Atlantic to re-evaluate the syn-rift and early post-rift geological context of sedimentary basin formation.
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
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
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 » Georges Bank Research & Data
Georges Bank Research & Data
January 2019
Georges Bank is a large submarine bank (250km by 150km – 40,000 km2) located at the edge of the Atlantic continental shelf between Cape Cod and Nova Scotia.
Nova Scotia Tidal Research Summary Report – Researching Tidal Energy – Marine Life: The Nova Scotia Experience
October 2015 – May 2016
This report looks at the extensive tidal energy-related research undertaken in the Bay of Fundy over a 10 year period beginning in 2005.