Abstract
Networks of halite veins have been analysed along galleries of the potash Cabanasses mine (Súria anticline, SE Pyrenees). The presence of a shape preferred orientation cross-cut by halite veins suggests that the rocks hosting the veins underwent ductile deformation before fracture formation and healing. The petrographical characteristics of veins and host rocks, as well as the analysis of their bromine content, reveal that the vein-forming fluids likely resulted from pressure-solution and dynamic recrystallisation of the Lower Halite Unit rocks. Fluids at high pressure migrated upwards and were arrested at the Halite-Sylvinite Unit causing fracture formation below the Potash Unit, which acted as a seal and did not experience brittle deformation.
| Original language | English |
|---|---|
| Title of host publication | Selected Studies in Geophysics, Tectonics and Petroleum Geosciences - Proceedings of the 3rd Conference of the Arabian Journal of Geosciences CAJG-3 |
| Editors | Sami Khomsi, Mourad Bezzeghoud, Santanu Banerjee, Mehdi Eshagh, Ali Cemal Benim, Broder Merkel, Amjad Kallel, Sandeep Panda, Haroun Chenchouni, Stefan Grab, Maurizio Barbieri |
| Publisher | Springer Nature |
| Pages | 111-114 |
| Number of pages | 4 |
| ISBN (Electronic) | 978-3-031-43807-3 |
| ISBN (Print) | 9783031438066 |
| DOIs | |
| Publication status | Published - 2024 |
Publication series
| Name | Advances in Science, Technology and Innovation |
|---|---|
| ISSN (Print) | 2522-8714 |
| ISSN (Electronic) | 2522-8722 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 7 Affordable and Clean Energy
Keywords
- Bromine
- Halite veins
- Hydrofracture
- Permeability
- Subsurface salt
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