Abstract
Structural, petrological and geochemical data allow us to constrain the fluid flow system at the frontal part of the Bóixols thrust sheet, Southern Pyrenees, focusing on the fluid origin, pathways and regimes. Throughout the evolution process of the fault-related Bóixols anticline, different fracture sets have been developed and mineralized with at least four generation of calcite cements. Such developments testify that such structures allowed the migration and interaction of four types of fluids during the early contraction, the syn folding stage and the latest folding stages.
Original language | English |
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Title of host publication | Advances in Science, Technology and Innovation |
Publisher | Springer Nature |
Pages | 219-221 |
Number of pages | 3 |
DOIs | |
State | Published - 2019 |
Externally published | Yes |
Publication series
Name | Advances in Science, Technology and Innovation |
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ISSN (Print) | 2522-8714 |
ISSN (Electronic) | 2522-8722 |
Bibliographical note
Publisher Copyright:© Springer Nature Switzerland AG 2019.
Keywords
- Bóixols anticline
- Fluid migration
- Fractures
- Southern pyrenees
ASJC Scopus subject areas
- Architecture
- Renewable Energy, Sustainability and the Environment
- Environmental Chemistry