RT Journal Article
T1 Validez e interpretación de los datos geotermométricos de los esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)
T1 Validity and interpretation of the geothermometric data of the zircon-bearing chlorite schists in the RondaPeridotites (Betic Cordilleras)
A1 Esteban, José Julián
A1 Cuevas, Julia
A1 Tubía, José María
AB This work reports the most precise geochemical compositions and geothermometric calculations of zirconbearingchlorite schists located at the south-western part of the Sierra Bermeja peridotite massif. Thecombination of electron microprobe and X-ray diffraction analysis shows the lack of interstratificationswithin chlorite IIb and allow us the use conventional geothermometers in the calculations of chloriteformation temperatures. Moreover, the application of geothermometers that do not depend on the SiO2composition of the host rock give us a new value ranges between 289-322 ºC for the chlorite schistsformation during the serpentinization of the R onda peridotites
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8539
UL http://hdl.handle.net/10272/8539
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026