The evaluation of drilling prospects is frequently based on seismic amplitude anomalies. To decipher "true" seismic prospects from "false" ones, we used...
The Beaufort-Mackenzie fold and thrust belt in Arctic Canada corresponds to the offshore part of the Cordilleran orogen in Yukon and Alaska. Previous tectonic...
The 15-km-long Matane pockmark train belongs to a series of NNE-striking alignments of pockmarks mapped on the seafloor of the St. Lawrence Estuary. It...
Density and surface tension of slag are important properties for mineral processing, metal processing, slagging combustion and slagging gasification. In the...
A new surficial geology map of the St. Lawrence River Estuary illustrates sediment distribution and variability in a relatively confined environment. This map...
The state of the interface between slag and carbon determines the slag foaming behavior and thus the effectiveness of carbon in electric arc furnace (EAF)...
Seismic wave propagation through the subsurface is characterized by a loss of high frequency energy that is desired for high-resolution imaging at depth. This...
This study documents two potential neotectonic features in the seismically active St. Lawrence estuary and western part of the Gulf of St. Lawrence of Quebec...
The seabed of the St. Lawrence Estuary is characterized by many fluid releasing features. On multibeam bathymetric images these features correspond to...
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