Metastable garnet in oceanic crust at the top of the lower mantle-Reference-Cited by-同舟云学术

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Metastable garnet in oceanic crust at the top of the lower mantle

Published:2002-12 Issue:6917 Volume:420 Page:803-806
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

Kubo Tomoaki,Ohtani Eiji,Kondo Tadashi,Kato Takumi,Toma Motomasa,Hosoya Tomofumi,Sano Asami,Kikegawa Takumi,Nagase Toshiro

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/nature01281.pdf

Reference28 articles.

1. Hirose, K., Fei, Y., Ma, Y. & Mao, H. K. The fate of subducted basaltic crust in the Earth's lower mantle. Nature 397, 53–56 (1999)

2. Akaogi, M. & Ito, E. Calorimetric study on majorite-perovskite transition in the system Mg4Si4O12-Mg3Al2Si3O12: transition boundaries with positive pressure-temperature slopes. Phys. Earth Planet. Inter. 114, 129–140 (1999)

3. Irifune, T. & Ringwood, A. E. Phase transformations in subducted oceanic crust and buoyancy relationships at depths of 600-800 km in the mantle. Earth Planet. Sci. Lett. 117, 101–110 (1993)

4. Ringwood, A. E. Role of the transition zone and 660 km discontinuity in mantle dynamics. Phys. Earth Planet. Inter. 86, 5–24 (1994)

5. Kesson, S. E., Fitz Gerald, J. D. & Shelley, J. M. G. Mineral chemistry and density of subducted basaltic crust at lower-mantle pressures. Nature 372, 767–769 (1994)

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