A volcano reawakens after more than 100,000 years of “silent” magma reservoir growth
O) from a highly metasomatized mantle. These volatile-rich magmas undergo water saturation and crystallize during ascent, preventing eruption. Such trapping mechanisms can grow large magma reservoirs and may enable transitions from small stratovolcanoes to highly hazardous, caldera-forming systems.
Authors
- Răzvan‐Gabriel Popa (ORCID: https://orcid.org/0000-0002-6344-8406)
- Olivier Bachmann (ORCID: https://orcid.org/0000-0003-2952-3465)
- Andrea Giuliani (ORCID: https://orcid.org/0000-0002-6823-2807)
- Marcel Guillong (ORCID: https://orcid.org/0000-0002-6920-3362)
Institutions
- Planetary Science Institute (US)
- Carnegie Institution for Science (US)
- ETH Zurich (CH)
Publication Details
- Journal
- Science Advances
- Published
- 2026-04-22
- DOI
- https://doi.org/10.1126/sciadv.aec9565
- Primary Topic
- Geological and Geochemical Analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung