Abstract
Discusses important constraints on the history of deep-water circulation and sedimentation in response to Cenozoic climatic change, as well as the tectonic evolution of the region. Not surprisingly, many of the Labrador Sea deep-circulation events correspond closely to major North Atlantic events and to important global climatic and paleoceanographic events, but a major drift-building episode may have occurred later in the Labrador Sea than it did in either the eastern North Atlantic or the western North Atlantic. -from Authors
Original language | English (US) |
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Pages (from-to) | 957-988 |
Number of pages | 32 |
Journal | Unknown Journal |
DOIs | |
State | Published - 1989 |
All Science Journal Classification (ASJC) codes
- General Environmental Science
- General Earth and Planetary Sciences