(Q59014815)

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Mechanism of the γ–β phase transformation of Mg2SiO4 at high temperature and pressure

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Mechanism of the γ–β phase transformation of Mg2SiO4 at high temperature and pressure (English)

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D. C. Rubie

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1

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A. J. Brearley

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2

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English

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publication date

December 1990

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Nature

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volume

348

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issue

6302

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page(s)

628-631

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A new self-organizing mechanism for deep-focus earthquakes

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7 January 2021

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A spinel to β-phase transformation mechanism in (Mg,Fe)2SiO4

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https://api.crossref.org/works/10.1038%2F348628A0

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Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications

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Stress dependence of the mechanism of the olivine–spinel transformation

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A temperature profile of the mantle transition zone

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Acoustic emissions and shear instabilities during phase transformations in Si and Ge at ultrahigh pressures

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The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgOFeOSiO2

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https://api.crossref.org/works/10.1038%2F348628A0

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7 January 2021

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10.1038/348628A0

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1043633422

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release_wh76ws7uefawpphjskkqyap324

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(Q59014815)

Mechanism of the γ–β phase transformation of Mg2SiO4 at high temperature and pressure

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