Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge-Reference-Cited by-同舟云学术

Neogene overflow of Northern Component Water at the Greenland-Scotland Ridge

Published:2006-06 Issue:6 Volume:7 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Poore H. R.¹,Samworth R.²,White N. J.¹,Jones S. M.³,McCave I. N.¹

Affiliation:

1. Department of Earth Sciences; University of Cambridge; Downing Street,; Cambridge; CB2 3EQ; UK

2. Statistical Laboratory, Centre for Mathematical Studies; University of Cambridge; Wilberforce Road,; Cambridge; CB3 0WB; UK

3. Department of Geology, Trinity College; University of Dublin; Dublin 2; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference117 articles.

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3. Late Miocene through early Pliocene deep water circulation and climate change viewed from the sub-Antarctic South Atlantic;Billups;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2002

4. Early Pliocene deep-water circulation: Stable isotope evidence for enhanced Northern Component Deep Water;Billups;Proc. Ocean Drill. Program Sci. Results,1997

5. Early Pliocene deep water circulation in the western equatorial Atlantic: Implications for high-latitude climate change;Billups;Paleoceanography,1998

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