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Ongoing deep deflation below Vesuvio coupled with Campi Flegrei uplift

Autor: Amoruso, A., Acocella, V., Crescentini, L.

Publikováno v: XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)

Adjacent volcanoes may influence each other’s activity; nevertheless, the extent and degree of this interaction, and how this may affect any eruption, remain poorly defined. Although Campi Flegrei and Vesuvio volcanoes are only 25 km apart, on oppo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::19a5b60811b5331e18b4667ef72f8960

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Akademický článek

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Relating Dike Geometry and Injection Rate in Analogue Flux-Driven Experiments

Autor: Galetto F, Bonaccorso A, Acocella V.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::9b819e328a0a3fb69d71246aeee1b0a5
https://hdl.handle.net/11590/393136

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Stress fields around magma chambers influenced by elastic thermo-mechanical deformation: implications for forecasting chamber failure

Autor: Browning J., Karaoğlu Ö., Bayer Ö., Turgay M. B., Acocella V.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::e0c3afdbdaa0376751e4061c1d090d98
https://hdl.handle.net/11590/393137

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Akademický článek

Dike emplacement and flank instability at Mount Etna: Constraints from a poro-elastic-model of flank collapse

Autor: Battaglia, M., Di Bari, M., Acocella, V., Neri, M.

Publikováno v: In Journal of Volcanology and Geothermal Research 2011 199(1):153-164

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Stress inversions to forecast magma pathways and eruptive vent location

Autor: Rivalta, E., Corbi, F., Passarelli, L., Acocella, V., Davis, T., Di Vito, M. A.

Publikováno v: Science Advances

We forecast where magma will breach Earth’s surface based on how the volcano’s shape and size have evolved.
When a batch of magma reaches Earth’s surface, it forms a vent from which volcanic products are erupted. At many volcanoes, success

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=pmid_dedup__::dc762753d0d1b4b4e02a98747ed015a1
https://gfzpublic.gfz-potsdam.de/pubman/item/item_4489888_3/component/file_4504898/4489888.pdf

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Megathrust earthquakes and the growth of NW-trending volcanic systems in the Southern Central Andes

Autor: Lupi M., Trippanera D. Gonzalez D., D’ Amico S., Acocella V., Cabello C., Stef M. M., Tassara A.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::d63ce2009c6c41e8895684e137fdf601
https://hdl.handle.net/11590/362392

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The 2008 eruptive unrest at Cerro Azul volcano (Galápagos) revealed by InSAR data and a new method for geodetic modelling

Autor: Galetto F., Hooper A., Bagnardi M., Acocella V.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3668::18b18534cc365734c19457ed6fdbb4ce
https://hdl.handle.net/11590/362393

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Sharing experimental data and facilities in EPOS: Updates on services for the analogue modelling community in the TCS Multi-scale Laboratories

Autor: Willingshofer, E., Funiciello, F., Rosenau, M., Schreurs, G., Zwaan, F., Buiter, S., ter Maat, G., Lange, O., Elger, K., Faccenna, C., Acocella, V., Reitano, R., Mastella, G., Guillaume, B., Corbi, F., EPOS TCS MSL analogue modelling team

Publikováno v: Abstracts

EPOS, the European Plate Observing System, is a unique e-infrastructure and collaborative environment for the solid earth science community in Europe and beyond. A wide range of world-class experimental (analogue modelling and rock and melt physics)

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::88279bd50907b96e456fa1d48d77f49a
https://doi.org/10.5194/egusphere-egu21-16301

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