Characteristics and evolution of the segmentation of the Mid-Atlantic Ridge between 20°N and 24°N during the last 10 million years
- 1 January 1995
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 129 (1-4) , 55-71
- https://doi.org/10.1016/0012-821x(94)00233-o
Abstract
No abstract availableKeywords
This publication has 38 references indexed in Scilit:
- Mantle flow patterns at an oceanic spreading centre: The Oman peridotites recordPublished by Elsevier ,2003
- Emplacement of deep crustal and mantle rocks on the west median valley wall of the MARK area (MAR, 23°N)Published by Elsevier ,2003
- An example of a recent accretion on the Mid-Atlantic Ridge: the Snake Pit neovolcanic ridge (MARK area, 23°22′N)Tectonophysics, 1991
- Segmentation of the Mid-Atlantic Ridge between 24° N and 30°40' NNature, 1990
- Alpine Jurassic ophiolites resemble the modern central Atlantic basementGeology, 1990
- Structural mapping in the Oman ophiolites: Mantle diapirism along an oceanic ridgeTectonophysics, 1988
- International Geomagnetic Reference Field revision 1987Eos, 1988
- Along-axis variations in seafloor spreading in the MARK areaNature, 1987
- Segmentation of mid-ocean ridgesNature, 1985
- A mechanism for magmatic accretion under spreading centresNature, 1984