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Geoscience » Source Rock & Depositional Environment

Central Atlantic Paleo-Oceans and Climates (CAPOC) (part of the PAGEO research program)

December 2020 – December 2022

CAPOC aims to develop the first integrated and high resolution biostratigraphic and isotopic proxy correlation for key intervals of the Jurassic/Cretaceous across the Central Atlantic conjugate margin.

Geoscience » Source Rock & Depositional Environment

Palaeobathymetry and Tectonic Evolution of Lower Jurassic Source Rocks of the Conjugate Nova Scotia-Moroccan Margins (part of the PAGEO research program)

December 2020 – July 2022

This project will address key questions related to the formation processes, structure and subsidence history of the Nova Scotia rifted margin, which are relevant to constrain the Upper Triassic to Jurassic palaeogeography and petroleum systems offshore Nova Scotia.

Geoscience » Source Rock & Depositional Environment

A Spatiotemporal Analysis of Paleobiogeographic Data to Constrain the Timing of Oceanic Connections between the Atlantic, Tethyan, and Pacific domains (part of the PAGEO research program)

November 2020 – May 2022

This project is based on a large-scale collection of previously generated Jurassic and Early Cretaceous nannofossil biostratigraphic data and aims to apply both traditional micropaleontological methods and modern data science methodologies to the in-depth analysis of that large dataset.

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.

Multi-Scale Turbulence Measurement in the Aquatron Laboratory

July 2018 – July 2019

This project has two primary objectives - to characterize the flow and turbulence in the Aquatron facility pool tank using turbulence sensors calibrated against a traceable standard; and to test technologies for investigating the horizontal variability of turbulence in real-world tidal channels.

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

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

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.

Remote Acoustic Measurements of Turbulence in High-Flow Tidal Channels during High Wave Conditions

April 2018 – April 2019

Many of the high-flow tidal channels targeted for worldwide in-stream hydro-electric development are impacted by surface gravity waves incident from a large exterior basin (e.g. the Bay of Fundy/Gulf of Maine/North Atlantic).

Turbine Wake Characterization

November 2017 – March 2019

Turbine wake characterization is a key endeavour to the development of in-stream tidal turbine arrays.  In a sense, a turbine’s footprint includes its wake, wherein flow speeds are less and turbulence is elevated compared to the ambient surroundings.  It is thus desired to not just delineate wake