Pressure generation in the Kawai-type multianvil apparatus and rheology of the Earth's interior
Author:
Affiliation:
1. Institute for Planetary Materials, Okayama University
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/49/1/49_191226/_pdf
Reference67 articles.
1. Alboussière, T., Deguen, R. and Melzani, M. (2010): Melting-induced stratification above the Earth's inner core due to convective translation. Nature, 466, 744-747.
2. Anzellini, S., Dewaele, A., Mezouar, M., Loubeyre, P. and Morard, G. (2013): Melting of Iron at Earth's Inner Core Boundary Based on Fast X-ray Diffraction. Science, 340, 464-466.
3. Belyakov, A., Sakai, T., Miura, H., Kaibyshev. R. and Tsuzaki, K. (2002): Continuous recrystallization in austenitic stainless steel after large strain deformation. Acta Mater., 50, 1547-1557.
4. Biggin, A.J., Piispa, E.J., Pesonen, L.J., Holme, R., Paterson, G.A., Veikkolainen, T. and Tauxe, L. (2015): Palaeomagnetic field intensity variations suggest Mesoproterozoic inner-core nucleation. Nature, 526, 245-248.
5. Brandon, A.D., Walker, R.J., Puchtel, I.S., Becker, H., Humayun, M. and Revillon, S. (2003): 186Os-187Os systematics of Gorgona Island komatiites: implications for early growth of the inner core. Earth Planet. Sci. Lett., 206, 411-426.
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