1-1-1-1-1-1-1-1-1-1-1-1-1-1 From: Lea Ostorero <leaemma.ostorero@xxxxxxxxx> Dear volcanology community, *apologies for cross-posting* We would like to invite you to submit your abstract to our session â??Tick, tickâ?¦ Boom! Timescales and dynamics of volcanic plumbing systems revealed by multidisciplinary approachesâ?? at the next IAVCEI Scientific Assembly 2025, which will be held in Geneva between June 29th and July 4th 2025. The session is aimed at exploring volcanic pre-eruptive timescales and magma dynamics. We particularly welcome multidisciplinary contributions from researchers worldwide, especially early-career researchers, correlating petrological and geochemical observations, experimental petrology, thermodynamic modeling and machine learning techniques, with monitoring signals. Please find below some more details about our session. The deadline to submit your abstract is December 20th 2024: https://on-line-form.eu/iavcei2025sa/abstracts/index.php?coo=1 <https://urldefense.com/v3/__https://on-line-form.eu/iavcei2025sa/abstracts/index.php?coo=1__;!!IKRxdwAv5BmarQ!dR6pMHpigmumvpxHZM30TMcYOYofYR4rPoVpK2pqQNVRED2oS7nbMDh1QLlkA8AdL3THYzqsA7B2KoVkrD3BRlxnRw$> We hope to see you in Geneva, Best regards, Lea Ostorero (University of Milano-Bicocca, Italy) on behalf of the conveners, Charline Lormand (University of Geneva, Switzerland); Alberto Caracciolo (NordVulk, Institute of Earth Sciences, University of Iceland); Simone Costa (INGV Pisa, Italy); Fidel Costa (Université Paris Cité, Institut de physique du globe de Paris, France) Tick, tickâ?¦ Boom! Timescales and dynamics of volcanic plumbing systems revealed by multidisciplinary approaches Conveners: Lea Ostorero, Charline Lormand, Alberto Caracciolo, Simone Costa, Fidel Costa Invited speaker: Euan Mutch (Earth Observatory of Singapore, Nanyang Technological University, Singapore) Understanding the timing of magma storage and the architecture of volcanic plumbing systems is crucial for unraveling the processes and timescales leading to eruptions. Substantial amounts of magma can assemble and ascend quickly, or may remain stored for years, centuries, or even longer and not erupt. What regulates the dynamics of magma storage versus eruption? How does magma transfer between different reservoirs at multiple depths eventually reach the surface? How are these processes recorded by monitoring signals? Direct observations of magma storage and transfer are impossible, and thus it is necessary to integrate the results from various methods to address these questions. We wish to gather cutting-edge findings from researchers worldwide, especially early-careers, to discuss the current understandings of magma mechanisms at depth. We particularly welcome multidisciplinary contributions correlating petrological and geochemical observations, such as fluid/melt inclusions studies, experimental petrology, thermodynamic modeling and machine learning techniques, with monitoring signals. 1-1-1-1-1-1-1-1-1-1-1-1-1-1 ------------------------------
