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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

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.

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.

Geoscience » Seismic & Marine Sound

Physics of the Interaction between a Crab and a Seismic Test Pulse – Development of a Mathematical Model and Testing of Model via Simulation

June 2009 – September 2011

Experimental attempts to establish whether seismic testing has any impact on crabs and the crab fishery have been hampered by a lack of theoretical work on the subject.

Geoscience » Source Rock & Depositional Environment

Development of Marginal Fields in Offshore Nova Scotia – Phase 1 & 2

June 2009 – June 2010

The reduction in cost of a marginal development is largely attributed to the potential reduction in size of the offshore installation. These types of installations are referred to as ‘minimal platforms’.

Mi’kmaq Ecological Knowledge Study (Phase 1)

August 2009

A Mi’kmaq Ecological Knowledge Study (MEKS) was conducted by Membertou Geomatics Consultants on the Minas Channel area of the Bay of Fundy. This is a comprehensive body of knowledge documenting the collective ecological knowledge held by the Mi’kmaq people.