Thermal effects of pyroxenites on mantle melting below mid-ocean ridges
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/s41561-018-0139-z.pdf
Reference56 articles.
1. Bonatti, E. et al. Mantle thermal pulses below the Mid-Atlantic Ridge and temporal variations in the formation of oceanic lithosphere. Nature 423, 499–505 (2003).
2. Brunelli, D., Seyler, M., Cipriani, A., Ottolini, L. & Bonatti, E. Discontinuous melt extraction and weak refertilization of mantle peridotites at the Vema lithospheric section (Mid-Atlantic Ridge). J. Petrol. 47, 745–771 (2006).
3. Bonatti, E. et al. Flexural uplift of a lithospheric slab near the Vema transform (central Atlantic): timing and mechanisms. Earth Planet. Sci. Lett. 240, 642–655 (2005).
4. Cipriani, A., Bonatti, E., Brunelli, D. & Ligi, M. 26 million years of mantle upwelling below a segment of the Mid Atlantic Ridge: the Vema lithospheric Section revisited. Earth Planet. Sci. Lett. 285, 87–95 (2009).
5. Cipriani, A., Brueckner, H. K., Bonatti, E. & Brunelli, D. Oceanic crust generated by elusive parents: Sr and Nd isotopes in basalt-peridotite pairs from the Mid-Atlantic Ridge. Geology 32, 657–660 (2004).
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