Silicon and oxygen isotopes unravel quartz formation processes in the Icelandic crust
7 1811 25 September 2017 12 March 2018 3 April 2018 5 11 4952 Next article >> 550 °C), hydrothermal high-temperature (~200-400 °C) quartz and low-temperature ( 550 °C), (2) hydrothermal (secondary) high-temperature quartz (~200 to 400 °C; n = 48) and (3) hydrothermal...Reply to Comment on “Ultra-high pressure and ultra-reduced minerals in ophiolites may form by lightning strikes” by Griffin et al., 2018: No evidence for transition zone metamorphism in the Luobusa ophiolite
C. Ballhaus, R.O.C. Fonseca, A. Bragagni 7 1810 06 January 2018 29 January 2018 9 March 2018 3 4 3815 Next article >> 12 GPa because it carries clinopyroxene exsolutions. In the Griffin et al. (2016a) Griffin, W.L., Afonso, J.C., Belousova, E.A., Gain, S.E., Gong,...