Abstract
Coast-parallel gabbro dikes in southwest Greenland have been dated as Jurassic; their distribution and age suggest that initial rifting between Greenland and Labrador took place at about the middle of the Mesozoic Era.
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W. Stuart Watt; The coast-parallel dike swarm of southwest Greenland in relation to the opening of the Labrador Sea. Canadian Journal of Earth Sciences 1969;; 6 (5): 1320–1321. doi: https://doi.org/10.1139/e69-133
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Coast-parallel gabbro dikes in southwest Greenland have been dated as Jurassic; their distribution and age suggest that initial rifting between Greenland and Labrador took place at about the middle of the Mesozoic Era.
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