Detachment tectonics at Mid-Atlantic Ridge 26°N
Author:
Funder
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
MEXT | Japan Agency for Marine-Earth Science and Technology
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-019-47974-z.pdf
Reference32 articles.
1. Cannat, M. Emplacement of mantle rocks in the sea or at mid-ocean ridges. J. of Geophys. Res. 98, 4163–4172 (1993).
2. Gente, P. et al. Characteristics and evolution of the segmentation of the Mid-Atlantic Ridge between 20°N and 24°N during the last 10 million years. Earth Planet. Sci. Lett. 129, 55–71 (1995).
3. Cannat, M. et al. Modes of seafloor generation at a melt-poor ultraslow spreading ridge. Geology 34, 605–608 (2006).
4. Smith, D. K., Cann, J. R. & Escartin, J. Widespread active detachment faulting and core complex formation near 13°N on the Mid-Atlantic Ridge. Nature 443, 440–444 (2006).
5. Schouten, H., Smith, D. K., Cann, J. R. & Escartín, J. Tectonic versus magmatic extension in the presence of core complexes at slow-spreading ridges from a visualization of faulted seafloor topography. Geology 38, 615–618, https://doi.org/10.1130/G30803.1 (2010).
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