p-T conditions and p-T paths of (ultra)high-pressure metapelites are important aspects in the study of (ultra)high-pressure metamorphism. This paper introduces several kinds of geothermobarometers applicable to (ultra)high-pressure metapelites, which include the garnet-phengite Fe^{2 +} -Mg exchange geothermometer, garnet-chlorite Fe^{2 +} -Mg exchange geothermometer, chloritoid-chlorite Fe^{2 +} -Mg exchange geothermometer, Si-in-phengite geobarometer, Zr-in-rutile geothermometer, Zr-in-titanite geothermobarometer, Ti-in-zircon geothermobarometer, Ti-in-quartz geothermobarometer and oxygen isotope geothermometer. In addition, a review is given concerning the applicable conditions and points for attention in use of the above geothermobarometers.