Zircon recycling and crystallization during formation of chromite- and Ni-arsenide ores in the subcontinental lithospheric mantle (Serranía de Ronda, Spain)

Zircon recycling and crystallization during formation of chromite- and Ni-arsenide ores in the subcontinental lithospheric mantle (Serranía de Ronda, Spain)

The ultramafic massifs of the Serranía de Ronda (namely Ronda, Ojén and Carratraca) are portions of Proterozoic (~1.2-1.8Ga) subcontinental lithospheric mantle (SCLM) affected by partial melting and infiltration of melts. The latter of these events was broadly coeval with the tectonic emplacement of...

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Bibliographic Details
Main Authors: González-Jiménez, J., Marchesi, C., Griffin, W., Gervilla, F., Belousova, E., Garrido, C., Romero, R., Talavera, Cristina, Leisen, M., O'Reilly, S., Barra, F., Martin, L.
Format: Journal Article
Published: Elsevier Science BV 2017
Online Access:http://hdl.handle.net/20.500.11937/52768

Internet

http://hdl.handle.net/20.500.11937/52768

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