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Volumn 101, Issue 3-4, 2011, Pages 217-224

Topotaxic relationships between spinel and pyroxene in kelyphite after garnet in mantle-derived peridotites and their implications to reaction mechanism and kinetics

Author keywords

[No Author keywords available]

Indexed keywords

CRYSTALLOGRAPHY; GARNET; MANTLE STRUCTURE; OLIVINE; PERIDOTITE; PYROXENE; REACTION KINETICS; SPINEL;

EID: 84880773874     PISSN: 09300708     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00710-011-0145-y     Document Type: Article
Times cited : (28)

References (14)
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  • 2
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  • 3
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  • 4
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    • Structural reasons for oriented intergrowth in some minerals
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    • Grunter, J.W.1
  • 5
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  • 7
    • 0025658718 scopus 로고
    • Thermobarometry, diffusion modelling and cooling rates of crustal garnet peridotites: Two examples from teh Moldanubian zone of the Bohemian Massif
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  • 8
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    • Formation and deformation mechanisms of pyroxene-spinel symplectite in an ascending mantle, the Horoman peridotite complex, Japan: An EBSD (electron backscatter diffraction) study
    • Odashima N, Morishita T, Ozawa K, Nagahara H, Tsuchiyama A, Nagashima R (2008) Formation and deformation mechanisms of pyroxene-spinel symplectite in an ascending mantle, the Horoman peridotite complex, Japan: an EBSD (electron backscatter diffraction) study. J Mineral Petrol Sci 103:1-15
    • (2008) J Mineral Petrol Sci , vol.103 , pp. 1-15
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  • 9
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.