RT Journal Article
T1 Rodingitización y formación de pectolita en diques graníticos de las Peridotitas de Ronda (Cordilleras Béticas, España)
T1 Rodingitization and pectolite development in granitic dykes from the Ronda peridotites (Betic Cordilleras, Spain)
A1 Esteban, José Julián
A1 Cuevas, Julia
A1 Tubía, José María
A1 Yusta, Iñaki
AB This work reports the local occurrence of rodingites formed from granitic dykes intrusive in the Ronda Peridotites. Representative mineral assemblages include chlorite, hydrogrossular, and prehnite but also pectolite, and xonotlite uncommon mineral in rodingites. In addition, some granitic dykes are characterized by the albitization of plagioclases. The development oflizardite in the adjacent serpentinites suggests that rodingitization was a low-temperature metasomatic process, which affects the granitic dykes in contact with peridotites during serpentinization
PB Sociedad Geológica de España
YR 2001
FD 2001
LK http://hdl.handle.net/10272/9725
UL http://hdl.handle.net/10272/9725
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026