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A unique electrical resistivity experiment reveals the 3D interior of Piton de la Fournaise

     Understanding the internal structure of volcanoes is essential for improving eruption predictions and assessing hazards. Achieving high-resolution 3D models of their interiors remains challenging. At Piton de la Fournaise, we used 3D electrical resistivity tomography to generate the first high-resolution image beneath the Terminal Cone, extending to one kilometer deep. Our model reveals a large hydrothermal zone beneath layered lava flows, with conductive offshoots extending toward the surface beneath the Bory crater and along faults linked to the Dolomieu crater. These results indicate that hydrothermal activity is strongly influenced by volcano-tectonic features at the summit. This study provides valuable insights into fluid circulation, magma transfer, and instability, offering a new framework for understanding the spatio-temporal evolution of Piton de la Fournaise and other volcanoes worldwide.

How to citehttps://doi.org/10.25519/w9j6-td91

Downloads and links
   DataFournaise_Inv_res.zip
   Metadata DataCite - XML - JSON
   Interoperable
   Repository
https://catalog.opgc.uca.fr/geonetwork2/srv/eng/catalog.search#/metadata/63914de8-e604-4356-93bd-81d0e0a36603
   Linkshttps://lmv.uca.fr/scan4volc/
   DOIhttps://doi.org/10.25519/W9J6-TD91 DOI

About this resource
   KeywordsGeology, Piton de la Fournaise, 3D electrical resistivity, Modeling, Hydrothermal system, Preferential fluid path, Dataset
   Ressource Type
Dataset
   LicenseCreative Commons Attribution 4.0 International
   Funding references
   CreatorsLydie-Sarah Gailler, Romain Guillard, Solène Buvat, Philippe Labazuy, Anthony Finizola, Roulleau Emilie
   Creation date
2024-05-05
   PublisherOPGC, LMV
   Publication year
2024

Technical information
   Spatial extent
   FormatsVTU, PVSM, MP4
   Software
   Lineage