Phase transition and density of subducted MORB crust in the lower mantle-Reference-Cited by-同舟云学术

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Phase transition and density of subducted MORB crust in the lower mantle

Published:2005-08 Issue:1-2 Volume:237 Page:239-251
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Hirose Kei,Takafuji Naoto,Sata Nagayoshi,Ohishi Yasuo

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Mineral chemistry and density of subducted basaltic crust at lower-mantle pressures;Kesson;Nature,1994

2. The fate of subducted basaltic crust in the Earth's lower mantle;Hirose;Nature,1999

3. Mineral assemblages of basalt in the lower mantle;Funamori;J. Geophys. Res.,2000

4. Mineralogy of subducted basaltic crust (MORB) from 25 to 37 GPa, and chemical heterogeneity of the lower mantle;Ono;Earth Planet. Sci. Lett.,2001

5. Subsolidus and melting phase relations of basaltic composition in the uppermost lower mantle;Hirose;Geochim. Cosmochim. Acta,2002

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3. Trace element partitioning in a deep magma ocean and the origin of the Hf-Nd mantle array;Science Advances;2024-08-16

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