The Labrador Sea formed during rifting between North America and Greenland beginning in the Early Cretaceous, with subsequent seafloor spreading from the...
The concept of a clinoform has been around for decades, but has received renewed attention in its application to stratigraphic studies. These morphological...
Sedimentary basins within the Labrador-Baffin Seaway are the product of rifting between Greenland and the paleo-North American Plate. Rifting started in the...
The evolution of the 2000 km long Mesozoic rift system underlying the Labrador-Baffin Seaway is described, with emphasis on results from geophysical data sets,...
The tectonic evolution of the Labrador-Baffin Seaway began with Early Cretaceous extension between Greenland and North America, resulting in the development of...
High quality seismic reflection data from the offshore Northern Labrador rifted margin allows imaging of the extended and rifted crust both along and across...
Studies of the structural deformation and the nature of the ocean-continent transition zone at the rifted continental margin, offshore central Labrador, and...
The Labrador-Baffin Seaway which includes the Labrador Sea, Davis Strait, and Baffin Bay began forming during Early Cretaceous rifting between the paleo-North...
Previous work in the Labrador Sea has led to development of the Labrador Sea Atlas (Bell, 1989), as well as lithostratigraphic, paleoenvironmental, and seismic...
Along the rifted northeast Newfoundland margin at the western termination of the Charlie-Gibbs Fracture Zone, we describe a previously unrecognised mid to Late...
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