Phase evolution in the Fe3O4-Fe2TiO 4 pseudo-binary system and its implications for remanent magnetization in Martian minerals

IEEE Transactions on Magnetics

Volumn 47, Issue 10, 2011, Pages 4124-4127

  Wise, Adam ^a   Saenko, Maryanna ^a   Velázquez, Amanda M ^a   Laughlin, David E ^a,b   Díaz Michelena, Marina ^c   McHenry, Michael E ^a  

^a CARNEGIE MELLON UNIVERSITY   (United States)

^b CARNEGIE MELLON UNIVERSITY   (United States)

^c INSTITUTO NACIONAL DE TÉCNICA AEROESPACIAL   (Spain)

Author keywords

Magnetic materials; magnetometry; Mars; phase separation; spinels

Indexed keywords

GROWTH KINETICS; IRON OXIDES; KINETICS; MAGNETIC MATERIALS; MAGNETITE; MAGNETIZATION; MAGNETOMETRY; MICROSTRUCTURE; MINERALS; PHASE SEPARATION; SOLID SOLUTIONS; TITANIUM COMPOUNDS;

DECOMPOSITION KINETICS; MAGNETIZATION MEASUREMENTS; MARS; METASTABLE SOLID SOLUTION; NUCLEATION AND GROWTH KINETICS; PSEUDO-BINARY SYSTEMS; REMANENT MAGNETIZATION; SPINELS;

SPINODAL DECOMPOSITION;

EID: 80053544568     PISSN: 00189464     EISSN: None     Source Type: Journal    
DOI: 10.1109/TMAG.2011.2157471     Document Type: Article

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