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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 » 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

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 » Play Fairway Analyses Atlases 2010–Present

Greater North Atlantic Liassic Petroleum Systems Synthesis

October 2019 – February 2020

In the absence of definitive, direct evidence for a Liassic (i.e. Lower Jurassic) petroleum system offshore Nova Scotia, information is required on source rock analogs around the greater North Atlantic region.

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 » Tectonics and Crustal Structure

Advanced Analyses of the MIRROR-1 OBS Profile from Offshore Morocco

July 2017 – April 2019

This project completes an analysis of the OETR and OCTOPUS seismic lines collected from offshore Nova Scotia and integrates the MIRROR I refraction line from offshore Morocco to allow comparison of the conjugate margins using wide-angle refraction/reflection ocean bottom seismometer profiles.

Geoscience » Play Fairway Analyses Atlases 2010–Present

Sydney Basin Play Fairway Analysis Atlas (2017)

July 2017

The objectives of this Play Fairway Analysis are to build a detailed and comprehensive understanding of the petroleum systems of the Sydney Basin and provide a resource evaluation based on the petroleum systems assessment.  The study concludes there is an effective petroleum system charged by mai

Geoscience » Tectonics and Crustal Structure

Extensional Tectonics across the Northern Nova Scotia Margin from Ocean Bottom Seismic Data

May 2015 – April 2017

This project analyzes two wide-angle refraction/reflection ocean-bottom seismometer profiles recently collected offshore north-central Nova Scotia.

Geoscience » Play Fairway Analyses Atlases 2010–Present

Central Scotian Slope Atlas (2016)

January – August 2016

The objective of this project was to identify and technically evaluate any significant exploration leads and prospects in the area of interest.  The study used integrated 3D basin modelling analysis to assess the timing of maturation of source rocks, transformation ratios, hydrocarbon entrapment,

Geoscience » Play Fairway Analyses Atlases 2010–Present

SW Nova Scotia Expansion Atlas (2015)

January 2015

This project is an expansion of the 2011 Play Fairway Analysis to the western border of the Nova Scotia marine shelf. This expansion corresponds to the Georges Bank zone and surrounding area extending from the Yarmouth Arch to the Shelburne Sub-basin.