Alkaline Silicate Metasomatism Recorded through Fe-Ti-Rich Mantle Xenoliths from the Calatrava Volcanic Field (Spain)

Alkaline Silicate Metasomatism Recorded through Fe-Ti-Rich Mantle Xenoliths from the Calatrava Volcanic Field (Spain)

Much of the lithospheric subcontinental mantle (SCLM) sampled in the Calatrava Volcanic Field (CVF) shows refertilization by alkaline metasomatic agents. The Cerro Pelado and El Palo ultramafic xenolith suites record the best evidence of this type of metasomatism in this volcanic field. Several grou...

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Bibliographic Details
Main Authors: Javier García Serrano, Carlos Villaseca, Cecilia Pérez-Soba, Manuel Jesús Román-Alpiste
Format: Article
Language:English
Published: MDPI AG 2024-02-01
Series:Minerals
Subjects:
alkaline metasomatism
peridotite xenoliths
pyroxenite xenoliths
Fe-Ti-rich wehrlites
websterite xenolith
subcontinental lithospheric mantle
Online Access:https://www.mdpi.com/2075-163X/14/3/241

Internet

https://www.mdpi.com/2075-163X/14/3/241

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