Journal
ANALYTICAL AND BIOANALYTICAL CHEMISTRY
Volume 397, Issue 7, Pages 2739-2752Publisher
SPRINGER HEIDELBERG
DOI: 10.1007/s00216-010-3831-4
Keywords
Raman spectroscopy; Thermoelastic model; Coesite; Quartz; Aragonite; Calcite
Funding
- Russian Foundation for Basic Research [10-05-00616-a, 10-05-00575-a]
- Russian Science Support Foundation
- Belgian Science Policy [P6/16]
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Raman-based geobarometry has recently become increasingly popular because it is an elegant way to obtain information on peak metamorphic conditions or the entire pressure-temperature-time (P-T-t) path of metamorphic rocks, especially those formed under ultrahigh-pressure (UHP) conditions. However, several problems need to be solved to get reliable estimates of metamorphic conditions. In this paper we present some examples of difficulties which can arise during the Raman spectroscopy study of solid inclusions from ultrahigh-pressure metamorphic rocks.
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