Research Portal
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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 » 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
Predictive Modeling of Sandstone Reservoir Distribution in the SW Scotian Basin
March 2018 – April 2020
The SW Scotian Basin is considered an under-explored passive margin sedimentary basin, however, it is also the most probable location to find oil on the Scotian Margin.
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 » Play Fairway Analyses Atlases 2010–Present
Shelburne Sub-Basin Play Fairway Analysis Update
November 2018 – June 2019
Shortly after the Scotian Shelf and Slope Play Fairway Analysis (PFA) was released in 2011, Shell Canada acquired six exploration parcels in the Shelburne Subbasin and collected approximately 10,850 square kilometers of wide azimuth 3D seismic data.
Geoscience » Source Rock & Depositional Environment
Nova Scotia-Morocco Conjugate Biostratigraphy Project
September 2018 – June 2019
Biostratigraphy, the study of fossils to determine the age and depositional conditions of the sediments from which they are recovered, is a critical input to the seismic reconstruction of the Nova Scotia and Morocco margins. Detailed biostratigraphical analyses have been completed by an internat
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.