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Volumn 102, Issue 1, 2007, Pages 57-60

Carbonic fluid inclusions in sapphirine + quartz bearing garnet granulite from the Limpopo Belt, southern Africa

Author keywords

Carbonic fluid inclusion; Granulite; Limpopo Belt; Sapphirine + quartz; Southern Africa

Indexed keywords


EID: 33947414871     PISSN: 13456296     EISSN: 13493825     Source Type: Journal    
DOI: 10.2465/jmps.060829     Document Type: Article
Times cited : (18)

References (13)
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  • 4
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    • Theoretical phase relations involving cordierite and garnet revisited: The influence of oxygen fugacity on the stability of sapphirine and spinel in the system Mg-Fe-Al-Si-O
    • Hensen, B.J. (1986) Theoretical phase relations involving cordierite and garnet revisited: the influence of oxygen fugacity on the stability of sapphirine and spinel in the system Mg-Fe-Al-Si-O. Contributions to Mineralogy and Petrology, 92, 362-367.
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  • 5
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    • Santosh, M.1    Tsunogae, T.2
  • 7
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  • 8
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    • Granulite facies metamorphism in the Central and Southern Marginal Zones of the Limpopo Belt, South Africa
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    • Tsunogae, T. and Miyano, T. (1989) Granulite facies metamorphism in the Central and Southern Marginal Zones of the Limpopo Belt, South Africa. Journal of the Geological Society of Japan, 95, 1-16 (in Japanese with English abstract).
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  • 10
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    • Tsunogae, T., Santosh, M., Osanai, Y., Owada, M., Toyoshima, T., Hokada, T. and Crowe, W.A. (2003) Fluid inclusions in an osumilite-bearing granulite from Bunt Island in the Archean Napier Complex, East Antarctica: implications for a decompressional P-T path? Polar Geoscience, 16, 61-75.
    • (2003) Polar Geoscience , vol.16 , pp. 61-75
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  • 11
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    • Tsunogae, T. and van Reenen, D.D. (2006a) Sapphirine + quartz corona around Mg-staurolite in garnet granulite from the Limpopo Belt, Southern Africa: evidence for ultrahigh-temperature metamorphism? 19th General Meeting of the International Mineralogical Association, Program & Abstracts, International Mineralogical Association, Japan, 211.
    • (2006) 19th General Meeting of the International Mineralogical Association , pp. 211
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  • 12
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  • 13
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.