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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

Tracking Mesozoic Paleoclimate Events on the Nova Scotia Margin: Integrating Biostratigraphic Legacy Data with New Stable Carbon Isotope Analyses (part of the PAGEO research program)

November 2020 – November 2021

This study will obtain empirical evidence for climatic perturbations and regional changes in oceanic circulation patterns by (1) acquiring an extensive dataset of stable isotope measurements from key wells located in the area of interest, (2) integrating these measurements with existing quantitat

Geoscience » Source Rock & Depositional Environment

Analysis of Palaeoenvironment, Palaeoclimate and Palaeooceanographic Models to Predict Distribution of Source Rocks Offshore Nova Scotia (part of the PAGEO research program)

November 2020 – June 2021

The objective of this work is to predict the distribution of Tithonian and early Jurassic (Toarcian, Pliensbachian, Sinemurian, Hettangian) source rocks based on biogeographic principles derived from modern environments, and palaeoenvironmental interpretations derived from palaeogeographic mappin

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

Sequence stratigraphy, titania diagenesis and relationship to petroleum systems modeling

October 2018 – January 2021

This project examines different forms of titania (TiO2) minerals to confirm the relationship between late diagenetic titania (i.e., titania minerals transformed under the heat and pressure of sedimentary processes) and hydrocarbon migration and thus assess the use of titania polymorphs as “pathfi

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.

Tidal Energy: Strategic Environmental Assessment – Bay of Fundy (Phase I)

April 2018

This Strategic Environmental Assessment (SEA) provides advice on whether, when and under what conditions tidal energy demonstration and commercial projects should be allowed in the Bay of Fundy.

Nova Scotia Small Tidal Test Centre: Gap Analysis and Business Case

November 2017 – March 2018

As the tidal energy industry develops, there is increasing interest in the prospects for small-scale tidal energy development. Building small-scale tidal energy installations has promise given the number of locations where they can be used.

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.