Ti-in quartz thermobarometry for Bhutan quartz mylonites

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.

石英中钛热压计（Ti-in-quartz thermobarometry，简称TitaniQ）基于钛在石英中的溶解度对压力和温度（P-T）的依赖性（Huang & Audetat, 2012；Kawasaki & Osanai, 2008；Ostapenko等, 1987；Ostapenko等, 2007；Thomas等, 2010；Wark & Watson, 2006）。所有微量元素测量均在斯坦福大学使用反向几何高分辨率灵敏离子探针（sensitive high-resolution ion microprobe reverse-geometry，简称SHRIMP-RG）完成。石英中钛数据用于解释主中央逆冲断层沿线石英糜棱岩的变形温度。