Asymmetric generation of oceanic crust at the ultra-slow spreading Southwest Indian Ridge, 64°E-Reference-Cited by-同舟云学术

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Asymmetric generation of oceanic crust at the ultra-slow spreading Southwest Indian Ridge, 64°E

Published:2007-05 Issue:5 Volume:8 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Searle R. C.¹,Bralee A. V.

Affiliation:

1. Department of Earth Sciences; Durham University; Durham; DH1 3LE; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. Magnetic polarity structure of the lower oceanic crust;Allerton;Geophys. Res. Lett.,2001

2. Extensional faulting and segmentation of the Mid-Atlantic Ridge north of the Kane fracture zone (24°00′N to 24°40′N);Allerton;Mar. Geophys. Res.,1995

3. Bathymetric segmentation and faulting on the Mid-Atlantic Ridge, 24°00′N to 24°40′N;Allerton;Geol. Soc. Spec. Publ.,1996

4. Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge-segments;Allerton;Geology,2000

5. Geology of the Atlantis Massif (Mid-Atlantic Ridge, 30°N): Implications for the evolution of an ultramafic oceanic core complex;Blackman;Mar. Geophys. Res.,2002

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3. The Global Spectrum of Seafloor Morphology on Mid‐Ocean Ridge Flanks Related to Magma Supply;Journal of Geophysical Research: Solid Earth;2023-11-29

4. Geophysical investigation of the Mado Megamullion oceanic core complex: implications for the end of back-arc spreading;Progress in Earth and Planetary Science;2023-07-14

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