High-pressure phase transitions of anorthosite crust in the Earth's deep mantle

Author:

Nishi MasayukiORCID,Gréaux Steeve,Tateno Shigehiko,Kuwayama Yasuhiro,Kawai Kenji,Irifune Tetsuo,Maruyama Shigenori

Funder

Grant-in-Aid for Scientific Research from the Japanese government

Ministry of Education and Science of the Russian Federation

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference79 articles.

1. Pyroxene-garnet solid-solution equilibria in the systems Mg4Si4O12-Mg3Al2Si3O12 and Fe4Si4O12-Fe3Al2Si3O12 at high pressures and temperatures;Akaogi;Physics of the Earth and Planetary Interiors,1977

2. Volatile accretion history of the terrestrial planets and dynamic implications;Albarede;Nature,2009

3. Density of MORB eclogite in the upper mantle;Aoki;Physics of the Earth and Planetary Interiors,2004

4. Why primordial continents were recycled to the deep: role of subduction erosion;Azuma;Geoscience Frontiers,2017

5. Coupled zircon Lu–Hf and U–Pb isotopic analyses of the oldest terrestrial crust, the >4.03 Ga Acasta Gneiss Complex;Bauer;Earth and Planetary Science Letters,2017

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