Causes and Consequences of Diachronous V-Shaped Ridges in the North Atlantic Ocean-Reference-Cited by-同舟云学术

Causes and Consequences of Diachronous V-Shaped Ridges in the North Atlantic Ocean

Author:

Parnell-Turner Ross¹^ORCID,White Nicky²^ORCID,Henstock Timothy J.³^ORCID,Jones Stephen M.⁴,Maclennan John²^ORCID,Murton Bramley J.⁵

Affiliation:

1. Department of Geology & Geophysics; Woods Hole Oceanographic Institution; Woods Hole MA USA

2. Bullard Laboratories, Department of Earth Sciences; University of Cambridge; Cambridge UK

3. National Oceanography Centre Southampton; University of Southampton; Southampton UK

4. School of Geography, Earth and Environmental Sciences; University of Birmingham; Edgbaston UK

5. National Oceanography Centre; Southampton UK

Funder

Natural Environment Research Council

Girdler Fund, University of Cambridge

BP Exploration

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference124 articles.

1. Channeling of plume flow beneath mid-ocean ridges;Albers;Earth and Planetary Science Letters,2001

3. Time variation in igneous volume flux of the Hawaii-Emperor hot spot seamount chain;Ark Van;Journal of Geophysical Research,2004

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