Reconstructing hydrothermal fluid pathways and storage at the Solfatara Crater (Campi Flegrei, Italy) using seismic scattering and absorption

dc.contributor.authorPilar Di Martino, Maria Del
dc.contributor.authorDe Siena, Luca
dc.contributor.authorSerlenga, Vincenzo
dc.contributor.authorDe Landro, Grazia
dc.date.accessioned2022-10-21T09:16:45Z
dc.date.available2022-10-21T09:16:45Z
dc.date.issued2022
dc.description.abstractImaging of fluid pathways is crucial to characterize processes taking place in hydrothermal systems, a primary cause of volcanic unrest and associated hazards. The joint imaging of seismic absorption and scattering is an efficient instrument to map fluid flow at crustal scale, and specifically in volcanoes; however, this technique has so far been applied to image volcanoes and hydrothermal systems at the kilometre scale. Here, we use data from a meter-scale, active seismic survey inside the shallow structure of the Solfatara crater to obtain the first frequency-dependent near-surface scattering and absorption model of a hydrothermal system. The Solfatara crater is the place used to monitor historic unrest at Campi Flegrei caldera (Italy), a high-risk volcano under continuous surveillance due to its closeness to a densely populated area. Improving the imaging of the shallow part of this system is crucial to broaden the understanding of unrest processes that are progressively characterizing other portions of the eastern caldera. The scattering contrasts highlight the primary structural feature, a fault separating the hydrothermal plume from zones of CO2 saturation nearing fumaroles. While high-absorption anomalies mark zones of high soil temperatures and CO2 fluxes, low-absorption anomalies indicate zones of very shallow upflow and are caused by contrasts between liquid-rich and vapour-rich fluids coming from mud pools and fumaroles, respectively. All maps show a SW-NE trend in anomalies consistent with fluid-migration pathways towards the eastern fumaroles. The results provide structural constraints that clarify mechanisms of fluid migration inside the crater. The techniques offer complementary geophysical images to the interpretation of hydrothermal processes and prove that seismic attenuation measurements are suitable to map fluid pathways in heterogeneous media at a detailed scale.en_GB
dc.description.sponsorshipGefördert durch die Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 491381577de
dc.identifier.doihttp://doi.org/10.25358/openscience-8074
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/8089
dc.language.isoengde
dc.rightsCC-BY-4.0*
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/*
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.titleReconstructing hydrothermal fluid pathways and storage at the Solfatara Crater (Campi Flegrei, Italy) using seismic scattering and absorptionen_GB
dc.typeZeitschriftenaufsatzde
jgu.journal.titleFrontiers in earth sciencede
jgu.journal.volume10de
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.nameJohannes Gutenberg-Universität Mainz
jgu.organisation.number7950
jgu.organisation.placeMainz
jgu.organisation.rorhttps://ror.org/023b0x485
jgu.pages.alternative852510de
jgu.publisher.doi10.3389/feart.2022.852510de
jgu.publisher.issn2296-6463de
jgu.publisher.nameFrontiers Mediade
jgu.publisher.placeLausannede
jgu.publisher.urihttps://www.frontiersin.org/articles/10.3389/feart.2022.852510/fullde
jgu.publisher.year2022
jgu.rights.accessrightsopenAccess
jgu.subject.ddccode550de
jgu.subject.dfgNaturwissenschaftende
jgu.type.contenttypeScientific articlede
jgu.type.dinitypeArticleen_GB
jgu.type.resourceTextde
jgu.type.versionPublished versionde

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