Dataset Information

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.

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 2022-09-25.

2020-03-04

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]

Natural Sciences and Engineering Research Council of Canada: NSERC

Coverage Scope: Regional (Continents, Oceans)
Geographic Location: Bhutan, Himalaya

geothermometry, daformation temperature, TitaniQ

2022-02-01

Collection