Ti-in quartz thermobarometry for Bhutan quartz mylonites

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
Ti-in-quartz thermobarometry (TitaniQ) is based on the pressure and temperature (P-T) dependence of the solubility of titanium in quartz (Huang & Audetat, 2012; Kawasaki & Osanai, 2008; Ostapenko et al., 1987; Ostapenko et al., 2007; Thomas et al., 2010; Wark & Watson, 2006). All trace element measurements were performed on the sensitive high-resolution ion microprobe reverse-geometry (SHRIMP-RG) at Stanford University. The Ti-in-Quartz data were interpreted in terms of deformation temperatures of quartz mylonites along the Main central Thrust.
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. Ti-in quartz thermobarometry for Bhutan quartz mylonites, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). https://doi.org/10.26022/IEDA/111508. Accessed 2024-05-27.
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: Regional (Continents, Oceans)
Geographic Location: Bhutan, Himalaya
User Contributed Keyword(s):
geothermometry, daformation temperature, TitaniQ
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