Extending the applicability of the Raman carbonaceous-material geothermometer using data from contact metamorphic rocks
The degree of graphitization of carbonaceous material (CM) has been widely used as an indicator of metamorphic grade. Previous work has demonstrated that peak metamorphic temperature (T) of regional metamorphic rocks can be estimated by an area ratio (R2) of peaks recognized in Raman spectra of CM....
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Veröffentlicht in: | Journal of metamorphic geology 2010-12, Vol.28 (9), p.895-914 |
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