The evolution of the footwall to the Ronda subcontinental mantle peridotites: insights from the Nieves Unit (western Betic Cordillera)

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The evolution of the footwall to the Ronda subcontinental mantle peridotites: insights from the Nieves Unit (western Betic Cordillera)

Strongly heterogeneous deformation and extreme metamorphic gradients characterize the dominantly carbonate Nieves Unit in the footwall to the Ronda mantle extrusion wedge in the western Betic Cordillera. A well-developed foliation and mineral lineation, together with isoclinal intrafolial folds, occ...

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Bibliographic Details
Main Authors:	Mazzoli, S., Martín-Algarra, A., Reddy, Steven, López Sánchez-Vizcaíno, V., Fedele, L., Noviello, A.
Format:	Journal Article
Published:	Geological Society Publishing House 2013
Subjects:	EBSD mantle peridotite deformation carbonates metamorphism
Online Access:	http://hdl.handle.net/20.500.11937/25240

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