Geophysical evidence for widespread Cenozoic bottom current activity from the continental margin of Nova Scotia, Canada-Reference-Cited by-同舟云学术

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Geophysical evidence for widespread Cenozoic bottom current activity from the continental margin of Nova Scotia, Canada

Published:2016-08 Issue: Volume:378 Page:237-260
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Calvin Campbell D.,Mosher David C.

Funder

Geological Survey of Canada

Offshore Energy Technical Research Association of Nova Scotia

Pengrowth-Nova Scotia Petroleum Innovation Grant

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference90 articles.

1. Anomalous bottom water south of the grand-banks suggests turbidity current activity;Amos;Science,1979

2. SEISMIC Stratigraphy and History of Deep Circulation and Sediment Drift Development in the Baffin Bay and the Labrador Sea;Arthur,1989

3. The Cenozoic ocean circulation based on ocean General Circulation Model results;Barron;Palaeogeography, Palaeoclimatology, Palaeoecology,1991

4. Suspended particulate loads and transports in the nepheloid layer of the abyssal Atlantic Ocean;Biscaye;Mar. Geol.,1977

5. A model for the growth of mudwaves in the presence of time varying currents;Blumsack;Deep-Sea Res. II,1993

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