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Eight good reasons why the uppermost mantle could be magnetic
Eric C. Ferré
,
Sarah A. Friedman
, Fatíma Martín-Hernández
, Joshua M. Feinberg
, Jessica L. Till
, Dmitri A. Ionov
, James A. Conder
Southern Illinois University
Universidad Complutense de Madrid
Instituto de Geociencias IGEO (UCM-CSIC), Fac. CC. Físicas
University of Minnesota Twin Cities
Institut de Minéralogie et de Physique des Milieux Condensés
National Centre for Scientific Research
Research output
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Contribution to journal
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Article
›
peer-review
85
Scopus citations
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Earth and Planetary Sciences
Xenolith
100%
Earth Surface
33%
Magnetic Anomaly
33%
Pyroxene
16%
Natural Remanent Magnetization
16%
Demagnetization
16%
Curie Temperature
16%
Tectonic Setting
16%
Fayalite
16%
Thermoremanent Magnetization
16%
Subduction Zone
16%
Remanence
16%
Craton
16%