Eight good reasons why the uppermost mantle could be magnetic

Tectonophysics

Volumn 624-625, Issue , 2014, Pages 3-14

  Ferré, Eric C ^a   Friedman, Sarah A ^a   Martín Hernández, Fatíma ^b,c   Feinberg, Joshua M ^d   Till, Jessica L ^e   Ionov, Dmitri A ^f   Conder, James A ^a  

^a SOUTHERN ILLINOIS UNIVERSITY   (United States)

^b UNIVERSIDAD COMPLUTENSE DE MADRID   (Spain)

^c INSTITUTO DE GEOCIENCIAS   (Spain)

^d UNIVERSITY OF MINNESOTA   (United States)

^e UNIVERSITÉ PIERRE ET MARIE CURIE   (France)

^f CNRS   (France)

Author keywords

Magnetic anomaly; Magnetite; Magnetization; Mantle; NRM; Xenolith

Indexed keywords

FERROMAGNETIC MATERIALS; FERROMAGNETISM; MAGNETIZATION; NATURAL RESOURCES MANAGEMENT; OLIVINE; OXYGEN; QUARTZ; REMANENCE; SILICATES;

MAGMATIC TEMPERATURES; MAGNETIC ANOMALIES; MANTLE; NATURAL REMANENT MAGNETIZATION; NRM; STOICHIOMETRIC MAGNETITE; THERMOREMANENT MAGNETIZATION; XENOLITH;

MAGNETITE;

MAGNETIC ANOMALY; MAGNETITE; MANTLE; NATURAL REMANENT MAGNETIZATION; THERMOREMANENT MAGNETIZATION; XENOLITH;

EID: 84901490723     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.tecto.2014.01.004     Document Type: Article

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