Petrofabric and seismic properties of lithospheric mantle xenoliths from the Calatrava volcanic field (Central Spain)
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文摘

The EBSD-based petrofabric study of peridotite xenoliths from the Neogene Calatrava volcanic field is presented.

The lherzolite mineral assemblage records crystal-plastic deformation and metasomatism by subduction-related melts.

The xenoliths exhibit various olivine fabrics that we ascribe to deformation in a suprasubduction mantle setting.

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