Unraveling the complexity of iron oxides at high pressure and temperature: Synthesis of Fe 5 O 6

Author:

Lavina Barbara1,Meng Yue2

Affiliation:

1. High Pressure Science and Engineering Center, University of Nevada, Las Vegas, Las Vegas, NV 89154–4002, USA.

2. High Pressure Collaborative Access Team, Carnegie Institution of Washington, Argonne, IL 60439–4803, USA.

Abstract

A novel iron oxide obtained at mantle’s conditions could play a critical role in processes shaping planets from their interiors.

Funder

Stewardship Science Academic Alliances

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference34 articles.

1. Introduction to oxygen fugacity and its petrologic importance;Frost B. R.;Rev. Mineral. Geochem.,1991

2. Discovery of the recoverable high-pressure iron oxide Fe4O5;Lavina B.;Proc. Natl. Acad. Sci. U.S.A.,2011

3. Nuclear forward scattering and first-principles studies of the iron oxide phase Fe4O5;Kothapalli K.;Phys. Rev. B,2014

4. In situ observation of the breakdown of magnetite (Fe3O4) to Fe4O5 and hematite at high pressures and temperatures;Woodland A. B.;Am. Mineral.,2012

5. Fe4O5 and its solid solutions in several simple systems;Woodland A. B.;Contrib. Mineral. Petrol.,2013

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