Mantle thermal structure and active upwelling during continental breakup in the North Atlantic-Reference-Cited by-同舟云学术

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Mantle thermal structure and active upwelling during continental breakup in the North Atlantic

Published:2001-08 Issue:3-4 Volume:190 Page:251-266
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Holbrook W.Steven,Larsen H.C.,Korenaga J.,Dahl-Jensen T.,Reid I.D.,Kelemen P.B.,Hopper J.R.,Kent G.M.,Lizarralde D.,Bernstein S.,Detrick R.S.

Publisher

Elsevier BV

Subject

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

Reference59 articles.

1. Origin of seaward-dipping reflectors in oceanic crust off the Norwegian margin by ‘subaerial sea-floor spreading’;Mutter;Geology,1982

2. Magmatism at rifted continental margins;White;Nature,1987

3. Magmatism at rift zones: The generation of volcanic continental margins and flood basalts;White;J. Geophys. Res.,1989

4. North Atlantic volcanic margins: Dimensions and production rates;Eldholm;J. Geophys. Res.,1994

5. South Atlantic volcanic margins;Gladczenko;J. Geol. Soc. Lond.,1997

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