Oxygen vacancy component (MgFeO<SUB>2.5</SUB>) produced by Fe<SUP>3+</SUP> in bridgmanite and its implications for viscosity variation in the mid-mantle

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    W[2019AGUFMDI31B0012K]
    LA["Linked Authors (0)"]
    LI["Linked Institutions (1)"]
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    W== affil ==>LI
    click LA "#linked-authors"
    click LI "#linked-institutions"

ADS bibcode

2019AGUFMDI31B0012K

year

2019

Listed Authors

Katsura, T.

Fei, H.

Liu, Z.

McCammon, C. A.

Listed Institutions

Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany; Center for High Pressure Science &amp; Technology Advanced Research, Beijing, China

Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany

Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany

Bayerisches Geoinstitut, University of Bayreuth, Bayreuth, Germany

Linked Authors [?]

Linked Institutions

• University of Bayreuth, Institute of Geophysics