Evidence of phyllosilicate alteration processes and clay mineral neoformation promoted by hydrothermal fluids in the Padul Fault area (Betic Cordillera, SE Spain)

1. Abad, I.
2. Nieto, F.
3. Reolid, M.
4. Jiménez-Millán, J.

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DOI: 10.1016/J.CLAY.2022.106669 GOOGLE SCHOLAR lock_openOpen access editor

Data source: Scopus