The Labrador water is just a northwestward expansion for the North Atlantic Ocean, through the Charlie-Gibbs break area within the south to Davis Strait within the north (Figure 2), which separates southern Greenland from Labrador. Rifting and breakup of the margins started through the Early Cretaceous (
85 Ma) according to borehole data (Balkwill 1990). Volcanics of Cretaceous and early Tertiary age onlap the rift structures and synrift sediments. A final period of intense volcanism in the Paleocene in the region of Davis Strait
60 Ma) is from the North Atlantic Magmatic Province (Gill et al., 1999). Unlike the Newfoundland and Nova Scotia margins towards the south, the pre-existing continental crust differs significantly with its many years and crustal properties: through the Paleozoic Appalachian Province into the south, through the belated Proterozoic Grenville Province into the Early Proterozoic Makkovik Province, and lastly the Archean Nain Province (Figure 9). A current summary of geophysical properties among these crustal units, centered on outcomes from the Lithoprobe ECSOOT system, is provided by Hall et al. (2002).
Figure 9. Maps for the Labrador margin showing (a) total sediment depth and (b) free-air gravity. Sedimentary basins and terranes that are continental
Following rifting, subsequent seafloor distributing within the Labrador water is documented by magnetic lineations (Roest and Srivastava, 1989), beginning first into the south throughout the belated Cretaceous (
70-80 Ma), then propagating towards the north and closing in the eocene that is late
40 Ma) when seafloor spreading ceased. A significant improvement in distributing happened at
55 Ma when rifting began Greenland that is separating from.
Ever looked at having an event with a woman that is married you may be also currently in one single? Then discover these 10 bits of advice to steer your action?
Considering An Affair With A Married Girl? Count The Fee
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