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This document discusses several geothermobarometry techniques used to determine pressure-temperature (P-T) conditions in metamorphic rocks, including: 1) The garnet-biotite exchange geothermometer which is based on the similar ionic radii of Fe and Mg allowing for temperature-dependent partitioning between garnet and biotite. 2) The GASP geobarometer which calculates pressure based on volume changes during garnet-biotite mixing. 3) Other techniques like the GRIPS and sphalerite geobarometers. 4) The

Author
Nextlevel Gaming
Language
EN