Raman spectroscopy on carbonaceous material in Bhutan

Grujic, Djordje; ORCID: 0000-0002-5833-8843
Ashley, Kyle T
Coble, Matthew A
Coutand, Isabelle
Kellett, Dawn A
Larson, Kyle P
Whipp, David M
Gao, Min
Whynot, Nicholas
The Raman spectroscopy on carbonaceous material (RSCM) geothermometer, was used to extract geothermometric data from the phyllites in the Lesser Himalayan Sequence in the eastern Bhutan. To determine the temperatures, interpreted as peak metamorphic temperatures, we used the calibration by Beyssac et al. (2002). Beyssac, O., Goffé, B., Chopin, C., & Rouzaud, J. N. (2002). Raman spectra of carbonaceous material in metasediments: a new geothermometer. Journal of Metamorphic Geology, 20(9), 859-871.
How to cite this dataset:
Grujic, D., Ashley, K. T., Coble, M. A., Coutand, I., Kellett, D. A., Larson, K. P., Whipp, D. M., Gao, M., Whynot, N., 2022. Raman spectroscopy on carbonaceous material in Bhutan, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111507. Accessed 2024-06-18.
DOI Creation Date:
Deformational temperatures across the Lesser Himalayan Sequence in eastern Bhutan and their implications for the deformation history of the Main Central Thrust. Tectonics, in press
Creative Commons Attribution-ShareAlike 4.0 International [CC-BY-SA-4.0]
Funding source(s):
Natural Sciences and Engineering Research Council of Canada: NSERC
Coverage Scope: Other
Geographic Location: Bhutan
User Contributed Keyword(s):
geothermometry, inverted metamorphic gradient, temperature gradient, Raman spectroscopy
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