Evidence of phyllosilicate alteration processes and clay mineral neoformation promoted by hydrothermal fluids in the Padul Fault area (Betic Cordillera, SE Spain)-Reference-Cited by-同舟云学术

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

Published:2022-11 Issue: Volume:230 Page:106669
ISSN:0169-1317
Container-title:Applied Clay Science
language:en
Short-container-title:Applied Clay Science

Author:

Abad Isabel,Nieto Fernando,Reolid Matías,Jiménez-Millán Juan

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference64 articles.

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3. From static alteration to mylonitization: a nano- to micrometric study of chloritization in granitoids with implications for equilibrium and percolation length scales;Airaghi;Contrib. Mineral. Petrol.,2020

4. Los Mantos Alpujárrides del tercio central de las Cordilleras Béticas. Ensayo de correlación tectónica de los Alpujárrides;Aldaya;Acta Geol. Hisp.,1979

5. Evidence for the activity and paleoseismicity of the Padul fault (Betic Cordillera, southern Spain);Alfaro;Acta Geol. Hisp.,2001

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