Fonte: Tschermaks Mineralogische und Petrographische Mitteilungen. Unidade: IGC
Assuntos: DOLOMITO, PETROLOGIA SEDIMENTAR
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SCHULTZ-GÜTTLER, Rainer Aloys. Correlation of the octahedral distortion angle of Mg-calcites and dolomites with excess enthalpies of mixing. Tschermaks Mineralogische und Petrographische Mitteilungen, v. 34, p. 271-277, 1985Tradução . . Disponível em: https://doi.org/10.1007/bf01082966. Acesso em: 26 set. 2024.APA
Schultz-Güttler, R. A. (1985). Correlation of the octahedral distortion angle of Mg-calcites and dolomites with excess enthalpies of mixing. Tschermaks Mineralogische und Petrographische Mitteilungen, 34, 271-277. doi:10.1007/bf01082966NLM
Schultz-Güttler RA. Correlation of the octahedral distortion angle of Mg-calcites and dolomites with excess enthalpies of mixing [Internet]. Tschermaks Mineralogische und Petrographische Mitteilungen. 1985 ; 34 271-277.[citado 2024 set. 26 ] Available from: https://doi.org/10.1007/bf01082966Vancouver
Schultz-Güttler RA. Correlation of the octahedral distortion angle of Mg-calcites and dolomites with excess enthalpies of mixing [Internet]. Tschermaks Mineralogische und Petrographische Mitteilungen. 1985 ; 34 271-277.[citado 2024 set. 26 ] Available from: https://doi.org/10.1007/bf01082966
