Three-dimensional magnetic stripes require slow cooling in fast-spread lower ocean crust
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
https://www.nature.com/articles/s41586-021-03831-6.pdf
Reference44 articles.
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3. Han, S. et al. Architecture of on- and off-axis magma bodies at EPR 9°37–40′N and implications for oceanic crustal accretion. Earth Planet. Sci. Lett. 390, 31–44 (2014).
4. Carbotte, S., Canales, J. P., Neimovic, M., Carton, H. & Mutter, J. Recent seismic studies at the East Pacific Rise 8°20′-10°10’N and Endeavour Segment: Insights into mid-ocean ridge hydrothermal and magmatic processes. Oceanography 25, 100–112 (2012).
5. VanTongeren, J. A., Kelemen, P. B. & Hanghøj, K. Cooling rates in the lower crust of the Oman ophiolite: Ca in olivine, revisited. Earth Planet. Sci. Lett. 267, 69–82 (2008).
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