Articles | Volume 11, issue 6
Solid Earth, 11, 2257–2281, 2020
https://doi.org/10.5194/se-11-2257-2020

Special issue: Faults, fractures, and fluid flow in the shallow crust

Solid Earth, 11, 2257–2281, 2020
https://doi.org/10.5194/se-11-2257-2020

Research article 25 Nov 2020

Research article | 25 Nov 2020

Influence of basement rocks on fluid evolution during multiphase deformation: the example of the Estamariu thrust in the Pyrenean Axial Zone

Daniel Muñoz-López et al.

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Cited articles

Arndt, M., Virgo, S., Cox, S. F., and Urai, J. L.: Changes in fluid pathways in a calcite vein mesh (Natih Formation, Oman Mountains): insights from stable isotopes, Geofluids, 14, 391–418, https://doi.org/10.1111/gfl.12083, 2014. 
Banks, D., Da Vies, G., Yardley, B. W., McCaig, A., and Grant, N.: The chemistry of brines from an Alpine thrust system in the Central Pyrenees: An application of fluid inclusion analysis to the study of fluid behaviour in orogenesis, Geochim. Cosmochim. Ac., 55, 1021–1030, https://doi.org/10.1016/0016-7037(91)90160-7, 1991. 
Baqués, V., Travé, A., Benedicto, A., Labaume, P., and Cantarero, I.: Relationships between carbonate fault rocks and fluid flow regime during propagation of the Neogene extensional faults of the Penedès basin (Catalan Coastal Ranges, NE Spain), J. Geochemical Explor., 106, 24–33, https://doi.org/10.1016/j.gexplo.2009.11.010, 2010. 
Baqués, V., Travé, A., Roca, E., Marin, M., and Cantarero, I.: Geofluid behaviour in successive extensional and compressional events: a case study from the southwestern end of the Valles-Penedes Fault (Catalan Coastal Ranges, NE Spain), Pet. Geosci., 18, 17–31, https://doi.org/10.1144/1354-079311-017, 2012. 
Barker, S. L. L. and Cox, S. F.: Evolution of fluid chemistry and fluid-flow pathways during folding and faulting: an example from Taemas, NSW, Australia, J. Geol. Soc. London, Spec. Publ., 359, 203–227, https://doi.org/10.1144/SP359.12, 2011. 
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Short summary
This study assesses the influence of basement rocks on the fluid chemistry during deformation in the Pyrenees and provides insights into the fluid regime in the NE part of the Iberian Peninsula.