@article{10272/8539,
year = {2006},
url = {http://hdl.handle.net/10272/8539},
abstract = {This work reports the most precise geochemical compositions and geothermometric calculations of zirconbearing
chlorite schists located at the south-western part of the Sierra Bermeja peridotite massif. The
combination of electron microprobe and X-ray diffraction analysis shows the lack of interstratifications
within chlorite IIb and allow us the use conventional geothermometers in the calculations of chlorite
formation temperatures. Moreover, the application of geothermometers that do not depend on the SiO2
composition of the host rock give us a new value ranges between 289-322 ºC for the chlorite schists
formation during the serpentinization of the R onda peridotites},
title = {Validez e interpretación de los datos geotermométricos de los esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)},
title = {Validity and interpretation of the geothermometric data of the zircon-bearing chlorite schists in the Ronda
Peridotites (Betic Cordilleras)},
author = {Esteban, José Julián and Cuevas, Julia and Tubía, José María},
}