Research Portal

Displaying 1 – 6 of 6 results

Filters

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.

Marine Renewable Energy Legislation – A Consultative Process

September 2010 – March 2011

This consultation paper focuses on Marine Renewable Energy legislation. It was developed to guide legislation related to the renewable energy resources in the Bay of Fundy before large-scale commercial development takes place.

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.