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Volume 2017 (2017), Article ID 8190109, 19 pages
Research Article

Fault-Related Controls on Upward Hydrothermal Flow: An Integrated Geological Study of the Têt Fault System, Eastern Pyrénées (France)

1Géosciences Montpellier, UMR 5243, Université de Montpellier, CNRS, Place Eugène Bataillon, 34095 Montpellier Cedex 5, France
2BRGM, ISTO, UMR 7327, 3 av. C. Guillemin, BP 36009, 45060 Orléans Cedex 2, France
3BRGM Occitanie-Site de Montpellier (Direction Régionale), 1039 rue de Pinville, 34000 Montpellier, France
4Calle Austria 2181, Asuncion, Paraguay

Correspondence should be addressed to Audrey Taillefer

Received 25 November 2016; Revised 8 March 2017; Accepted 23 April 2017; Published 2 August 2017

Academic Editor: Mark Tingay

Copyright © 2017 Audrey Taillefer et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

Supplementary Material

This Supplementary Material contains 4 appendices. In Appendix 1, the reader will find thin section pictures of the Têt fault core zone and of damage zone at Llo, Thues-entre-Valls and Thues-les-bains (Apprendix 1), with details on the cataclastic textures, carbonate and quartz veins and deformations kinematics. The detailled analysis of the Têt fault outcrop at Llo is available in Appendix 2. Appendix 3 gives details of the XRD-determined composition of the white sinter deposits described in the main text. Finally, field and thin section pictures of ductile fault-related deformation and deposits around the hot springs are described in Appendix 4.

  1. Supplementary Material