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Data DOI: 10.26022/IEDA/111508
Ti-in quartz thermobarometry for Bhutan quartz mylonites
  • Grujic, Djordje
  • 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., Coble, M., Coutand, I., Kellett, D., Larson, K., Whipp, D., Gao, M., Whynot, N. 2022. Ti-in quartz thermobarometry for Bhutan quartz mylonites, Version 1.0. Interdisciplinary Earth Data Alliance (IEDA). Accessed 2021-03-08.
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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