Artigo Revisado por pares

Origin and structure of the Iceland Plateau and Kolbeinsey Ridge

1972; American Geophysical Union; Volume: 77; Issue: 29 Linguagem: Inglês

10.1029/jb077i029p05688

ISSN

2156-2202

Autores

G. Leonard Johnson, J. R. Southall, P. Young, Peter Vogt,

Tópico(s)

Geological and Geophysical Studies

Resumo

Journal of Geophysical Research (1896-1977)Volume 77, Issue 29 p. 5688-5696 Origin and structure of the Iceland Plateau and Kolbeinsey Ridge G. L. Johnson, G. L. JohnsonSearch for more papers by this authorJ. R. Southall, J. R. SouthallSearch for more papers by this authorP. W. Young, P. W. YoungSearch for more papers by this authorP. R. Vogt, P. R. VogtSearch for more papers by this author G. L. Johnson, G. L. JohnsonSearch for more papers by this authorJ. R. Southall, J. R. SouthallSearch for more papers by this authorP. W. Young, P. W. YoungSearch for more papers by this authorP. R. Vogt, P. R. VogtSearch for more papers by this author First published: 10 October 1972 https://doi.org/10.1029/JB077i029p05688Citations: 44AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Abstract Recent geophysical data from the Iceland plateau have revealed that asymmetrical sea-floor spreading is apparently occurring on the mid-ocean ridge. The western (Greenland) side is spreading at an average half rate of 0.77 cm/year out to anomaly 5, whereas the eastern side is spreading at an average half rate of 0.82 cm/year. 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