- Abstract:
-
Here we show that the onset of deep water overflow from the Norwegian-Greenland Sea into the North Atlantic, interpreted to represent the onset of a modern-style North Atlantic Deep Water mass, commenced close to the early to middle Eocene boundary. This finding is based on the identification of a large, elongate contourite sediment drift, the "Judd Falls Drift," in the Faeroe-Shetland Basin, through detailed mapping of high-resolution two-dimensional and three-dimensional seismic data. This ...
Expand abstract - Publisher copy:
- 10.1130/G32461.1
-
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- Journal:
- Geology
- Volume:
- 40
- Issue:
- 3
- Pages:
- 255-258
- Publication date:
- 2012-03-05
- DOI:
- EISSN:
-
1943-2682
- ISSN:
-
0091-7613
- URN:
-
uuid:1175c863-6cbb-4d65-9040-04d0f4aa4fb1
- Source identifiers:
-
331795
- Local pid:
- pubs:331795
- Language:
- English
- Copyright date:
- 2012
Journal article
Onset of North Atlantic deep water production coincident with inception of the Cenozoic global cooling trend
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