Phase relation and mineral chemistry in pyrolite to 2200°C under the lower mantle pressures and implications for dynamics of mantle plumes

Author:

Nishiyama Norimasa1,Yagi Takehiko1

Affiliation:

1. Institute for Solid State Physics; University of Tokyo; Kashiwa Japan

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference68 articles.

1. The excess temperature of plumes rising from the core-mantle boundary;Albers;Geophys. Res. Lett.,1996

2. Evaluation of (Mg,Fe) partitioning between silicate perovskite and magnesiowüstite up to 120 GPa and 2300 K;Andrault;J. Geophys. Res.,2001

3. Equation of state of lower mantle (Al,Fe)-MgSiO3 perovskite;Andrault;Earth Planet. Sci. Lett.,2001

4. Iron-magnetism distribution coefficients between spinel [(Mg,Fe)2SiO4], magnesiowüstite [(Mg,Fe)O], and perovskite [(Mg,Fe)SiO3];Bell;Carnegie Inst. Washington Year Book,1979

5. High-pressure polymorphs of olivine and the 660-km seismic discontinuity;Chudinovkikh;Nature,2001

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