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Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition

Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2262079792

Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition

About this item

Full title

Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition

Publisher

Berlin/Heidelberg: Springer-Verlag

Journal title

Physics and chemistry of minerals, 2009-12, Vol.36 (10), p.585-592

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer-Verlag

More information

Scope and Contents

Contents

Recent high-pressure studies have shown that an electronic spin transition of iron in ferropericlase, an expected major phase of Earth’s lower mantle, results in changes in its properties, including density, incompressibility, radiative thermal conductivity, electrical conductivity, and sound velocities. To understand the rheology of ferropericlase...

Alternative Titles

Full title

Deformation of lower-mantle ferropericlase (Mg,Fe)O across the electronic spin transition

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2262079792

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2262079792

Other Identifiers

ISSN

0342-1791

E-ISSN

1432-2021

DOI

10.1007/s00269-009-0303-5

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