The evolution of the subcontinental mantle beneath the Central Iberian Zone: Geochemical tracking of its mafic magmatism from the Neoproterozoic to the Cenozoic

1. Villaseca, C.
2. Orejana, D.
3. Higueras, P.
4. Pérez-Soba, C.
5. García Serrano, J.
6. Lorenzo, S.

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DOI: 10.1016/J.EARSCIREV.2022.103997 GOOGLE SCHOLAR lock_openOpen access editor

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