Abstract The Campi Flegrei caldera in Southern Italy is one of the most populated active
volcanoes on Earth. It has an unprecedented record of historical unrest and eruption that …

As our ability to detect volcanic unrest improves, we are increasingly confronted with the
question of whether the unrest has a magmatic origin (magma on the move) or a non …

Volatile elements play an important role in many aspects of the physicochemical architecture
of sub-volcanic plumbing systems, from the liquid line of descent to the dynamics of magma …

Unrest at large calderas rarely ends in eruption, encouraging vulnerable communities to
perceive emergency warnings of volcanic activity as false alarms. A classic example is the …

The 501 m deep hole of the Campi Flegrei Deep Drilling Project, located west of the Naples
metropolitan area and inside the Campi Flegrei caldera, gives new insight to reconstruct the …

Several recent models that have been put forth to explain bradyseism at Campi Flegrei (CF),
Italy, are discussed. Data obtained during long‐term monitoring of the CF volcanic district …

The eruptions of Campi Flegrei (Southern Italy), one of the most studied and dangerous
active volcanic areas of the world, are fed by mildly potassic alkaline magmas, from …

Ambient noise polarizes inside fault zones, yet the spatial and temporal resolution of
polarized noise on gas-bearing fluids migrating through stressed volcanic systems is …

We report, for the first time, evidence of seismically induced soft‐sediment deformations in
the central area of the active Campi Flegrei caldera (southern Italy). We analyzed the marine …

Porphyry Cu deposits, the major source of many metals currently utilized by modern
civilization, form via the interplay between magmatism, tectonism, and hydrothermal …