Evolution of the Fluid System During the Formation of the Fault-Related Bóixols Anticline (Southern Pyrenees)

Nicholas Nardini, Daniel Muñoz-López*, David Cruset, Irene Cantarero, Juan Diego Martín-Martín, Anna Travé

*Corresponding author for this work

Research output: Chapter in Book/Report/Conference proceedingChapterpeer-review

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 languageEnglish
Title of host publicationAdvances in Science, Technology and Innovation
PublisherSpringer Nature
Pages219-221
Number of pages3
DOIs
StatePublished - 2019
Externally publishedYes

Publication series

NameAdvances in Science, Technology and Innovation
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

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