Atypical peri-Gondwanan granodiorite–tonalite magmatism from Southern Iberia. Origin of magmas and implications

An ensemble of fifteen granodiorite/tonalite plutons and minor intrusions was generated during CambroOrdovician times (ca. 498–462 Ma) at the margin of Gondwana, which occupies a large portion of the Central Iberian Zone of the Iberian Massif (Spain and Portugal). This ensemble is known as the Beira...

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Bibliographic Details
Main Author: Castro, A. (author)
Other Authors: Pereira, M.F. (author), Rodriguez, C. (author), Fernandez, C. (author), de la Rosa, J. (author)
Format: article
Language:eng
Published: 2022
Subjects:
tonalite-granodiorite
cambro-Ordovician magmatism
Iberia
Gondwana
Online Access:http://hdl.handle.net/10174/32757
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/32757

Internet

http://hdl.handle.net/10174/32757

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