Research Portal
Displaying 1 – 6 of 6 results
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.
Geoscience » Georges Bank Research & Data
Georges Bank Research & Data
January 2019
Georges Bank is a large submarine bank (250km by 150km – 40,000 km2) located at the edge of the Atlantic continental shelf between Cape Cod and Nova Scotia.
Geoscience » Source Rock & Depositional Environment
Predictive Modelling of Sandstone Reservoir Quality in the Scotian Basin
May 2016 – December 2018
This project uses existing knowledge of inferred drainage basin areas and paleoclimate to model multiple river inputs to the Scotian Basin. The modelled sedimentary succession is compared with actual sediment thicknesses in the basin.
Geoscience » Spill Preparedness
Advanced Coastal Mapping to Support Hydrodynamic Modelling
April 2016 – June 2018
Nova Scotia’s Atlantic coast exhibits a variety of shorelines that may be vulnerable to contamination in the event of an offshore oil spill. In turn, variable currents, changing water levels, shoals, and exposed seaside conditions make effective spill response difficult for tidal inlets.
Geoscience » Seismic & Marine Sound
Establishment of Baseline Biological Data on Snow Crab (Chionoecetes opilio) Offshore Cape Breton for Future Assessment of Potential Impacts of Seismic Noise on Snow Crab
April 2012 – February 2015
The study investigates the impact of sound energy generated by acoustic/seismic arrays on snow crabs.
Seasonal Erodibility of Sediment in the Upper Bay of Fundy
February 2012 – January 2015
This project developed methods for studying sedimentation to the macro-tidal flats of the upper Bay of Fundy. The researchers looked at seasonal variation in the erodibility of sediments in tidal creeks and flats using a Gust Erosion Chamber and repeated grain size surveys.