Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary-Reference-Cited by-同舟云学术

Buoyancy of slabs and plumes enhanced by curved post-garnet phase boundary

Published:2023-07-27 Issue:9 Volume:16 Page:828-832
ISSN:1752-0894
Container-title:Nature Geoscience
language:en
Short-container-title:Nat. Geosci.

Author:

Ishii Takayuki^ORCID,Frost Daniel J.,Kim Eun Jeong^ORCID,Chanyshev Artem^ORCID,Nishida Keisuke^ORCID,Wang Biao^ORCID,Ban Rintaro,Xu Jianing^ORCID,Liu Jin^ORCID,Su Xiaowan,Higo Yuji,Tange Yoshinori^ORCID,Mao Ho-kwang^ORCID,Katsura Tomoo^ORCID

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://www.nature.com/articles/s41561-023-01244-w.pdf

Reference56 articles.

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2. Christensen, U. R. & Yuen, D. A. Layered convection induced by phase transitions. J. Geophys. Res. Solid Earth 90, 10291–10300 (1985).

3. Tackley, P. J., Stevenson, D. J., Glatzmaier, G. A. & Schubert, G. Effects of an endothermic phase transition at 670 km depth in a spherical model of convection in the Earth’s mantle. Nature 361, 699–704 (1993).

4. Čížková, H. & Bina, C. R. Effects of mantle and subduction-interface rheologies on slab stagnation and trench rollback. Earth Planet. Sci. Lett. 379, 95–103 (2013).

5. Ballmer, M. D., Schmerr, N. C., Nakagawa, T. & Ritsema, J. Compositional mantle layering revealed by slab stagnation at ~1000-km depth. Sci. Adv. 1, e1500815 (2015).

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