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Volumn 13, Issue 5, 2001, Pages 871-881

Crystal-chemical reasons for the immiscibility of periclase and wüstite under lithospheric P, T condition

Author keywords

Heat treatment; Periclase; Repulsive interactions; W stite; X ray diffraction

Indexed keywords

ARSENIC COMPOUNDS; BINARY ALLOYS; BOND LENGTH; CHEMICAL ANALYSIS; ELECTRONIC PROPERTIES; ELECTROSTATICS; HEAT TREATMENT; IRON; IRON OXIDES; MAGNESIA; OXIDE MINERALS; POSITIVE IONS; SINGLE CRYSTALS; SOLID SOLUTIONS; X RAY DIFFRACTION;

EID: 0034804515     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2001/0013/0871     Document Type: Article
Times cited : (31)

References (36)
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  • 11
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    • Fei, Y.1    Mao, H.K.2
  • 15
    • 0001608329 scopus 로고
    • Stoichiometrich FeO as metastable intermediate of the decomposition of wüstite at 225° C
    • (1970) Z. Naturforsch , vol.25 , pp. 1996-1997
    • Hentschel, B.1
  • 29
    • 84944648082 scopus 로고
    • Revised effective ionic radii and systematic studies of interatomic distances in halides and chalcogenides
    • (1976) Acta Cryst , vol.32 A , pp. 751-767
    • Shannon, R.D.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.