Synthesis of inverse ringwoodite sheds light on the subduction history of Tibetan ophiolites
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-018-23790-9.pdf
Reference41 articles.
1. Griffin, W. L. et al. Mantle Recycling: Transition-Zone metamorphism of Tibetan ophiolitic peridotites and its tectonic implications. J. Petrol. 57, 655–684 (2016).
2. Satsukawa, T., Griffin, W. L., Piazolo, S. & O’Reilly, S. Y. Messengers from the deep: Fossil wadsleyite-chromite microstructures from the mantle Transition Zone. Sci. Rep. 5, 16484 (2015).
3. Binns, R. A., Davis, R. J. & Reed, S. J. B. Ringwoodite, natural (Mg, Fe)2SiO4 spinel in the Tenham meteorite. Nature 221, 943–944 (1969).
4. Ita, J. & Stixrude, L. Petrology, elasticity, and composition of the mantle transition zone. J. Geoph. Res. 97, 6849–6866 (1992).
5. Frost, D. J. The upper mantle transition zone. Elements 4, 171–176 (2008).
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