Research Portal
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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.
In Situ Turbulence Replication and Measurement (InSTREAM)
October 2015 – January 2018
The In Situ Turbulence Replication and Measurement (InSTREAM) project was conceived to address some fundamental questions about the turbulence physics in tidal energy sites and laboratory tanks used to simulate these sites.
Investigation of the Vertical Distribution, Movement and Abundance of Fish in the Vicinity of Proposed Tidal Power Energy Conversion Devices
March 2010 – December 2014
This project studied active fish avoidance of a turbine using the Coda Octopus Echoscope II 3-D multi-beam sonar mounted on a bottom platform. The objective was to observe and quantify the distribution and abundance of fish in the water column and their ability to detect and avoid turbines.
Atlantic Sturgeon Spatial and Temporal Distribution in Minas Passage, Nova Scotia, Canada, a Region of Future Tidal Energy Extraction
January 2010 – January 2014
In the Bay of Fundy, Atlantic sturgeon from endangered and threatened populations in the USA and Canada migrate through Minas Passage to enter and leave Minas Basin.
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.