Evidence of thermal-driven processes triggering the 2005–2014 unrest at Campi Flegrei caldera

G Chiodini, J Vandemeulebrouck, S Caliro… - Earth and Planetary …, 2015 - Elsevier
An accelerating process of ground deformation that began 10 years ago is currently affecting
the Campi Flegrei caldera. The deformation pattern is here explained with the overlapping of …

[HTML][HTML] Hydrothermal pressure-temperature control on CO2 emissions and seismicity at Campi Flegrei (Italy)

G Chiodini, S Caliro, R Avino, G Bini… - Journal of Volcanology …, 2021 - Elsevier
Fluids supplied by stored magma at depth are causal factors of volcanic unrest, as they can
cause pressurization/heating of hydrothermal systems. However, evidence for links between …

Stratigraphy, structure, and volcano-tectonic evolution of Solfatara maar-diatreme (Campi Flegrei, Italy)

R Isaia, S Vitale, MG Di Giuseppe, E Iannuzzi… - …, 2015 - pubs.geoscienceworld.org
This study focuses on the Solfatara volcano within Campi Flegrei, a volcanic field located on
the Tyrrhenian coast of southern Italy. Volcanism at the Campi Flegrei caldera has included …

Fluid accumulation zone by seismic attributes and amplitude versus offset analysis at Solfatara Volcano, Campi Flegrei, Italy

S Gammaldi, A Ismail, A Zollo - Frontiers in Earth Science, 2022 - frontiersin.org
The imaging of volcanic systems is a challenging topic that attracts the scientific community's
attention. The characterization of structures and rock properties by means of seismic active …

[HTML][HTML] Hydrothermal alteration of surficial rocks at Solfatara (Campi Flegrei): Petrophysical properties and implications for phreatic eruption processes

K Mayer, B Scheu, C Montanaro, TI Yilmaz… - Journal of Volcanology …, 2016 - Elsevier
Solfatara crater is located within the Campi Flegrei caldera to the west of Naples (Italy). It is
one of the largest fumarolic manifestations known, and the rocks hosting the hydrothermal …

Three‐dimensional electrical resistivity tomography of the Solfatara crater (Italy): Implication for the multiphase flow structure of the shallow hydrothermal system

M Gresse, J Vandemeulebrouck… - Journal of …, 2017 - Wiley Online Library
The Solfatara volcano is the main degassing area of the Campi Flegrei caldera,
characterized by 60 years of unrest. Assessing such renewal activity is a challenging task …

Volcano‐tectonic setting of the Pisciarelli fumarole field, Campi Flegrei caldera, southern Italy: Insights into fluid circulation patterns and hazard scenarios

R Isaia, MG Di Giuseppe, J Natale, FDA Tramparulo… - …, 2021 - Wiley Online Library
Phreatic and hydrothermal eruptions are small energetic explosive events that generally
have few to no precursors and represent a considerable hazard in tourist and urban areas …

Permeability of volcanic rocks to gas and water

MJ Heap, T Reuschlé, JI Farquharson… - Journal of Volcanology and …, 2018 - Elsevier
The phase (gas or liquid) of the fluids within a porous volcanic system varies in both time
and space. Laboratory experiments have shown that gas and water permeabilities can differ …

3D structure of the Campi Flegrei caldera central sector reconstructed through short-period magnetotelluric imaging

A Troiano, MG Di Giuseppe, R Isaia - Scientific Reports, 2022 - nature.com
Abstract The Campi Flegrei caldera experienced an unrest phase dating to 2005, which
primary expression is the impressive ground uplift, accompanied by increasing degassing …

Hydrothermal and magmatic system of a volcanic island inferred from magnetotellurics, seismicity, self‐potential, and thermal image: an example of Miyakejima …

M Gresse, M Uyeshima, T Koyama… - Journal of …, 2021 - Wiley Online Library
Phreatic and phreatomagmatic eruptions represent some of the greatest hazards occurring
on volcanoes. They result from complex interactions at a depth between rock, water, and …