Volcanic ash (tephra) erupted from the frequently active Campi Flegrei volcano forms layers
in many palaeoenvironmental archives across Italy and the Mediterranean. Proximal …

Abstract The Central Mediterranean region is one of the most important areas on Earth for
studying subduction-related potassic and ultrapotassic magmatism, derived from partial …

Italian Plio-Quaternary magmatism exhibits a very wide petrological, geochemical and
radiogenic-isotope variability, which makes magma genesis and geodynamic significance …

The results of a tephrochronological study on 340 distal tephra layers intercalated within
72.5 m of sediments in Lago Grande di Monticchio (southern Italy) are outlined. This maar …

Eruption forecasting and hazard assessments at the restless Campi Flegrei caldera, within
the Neapolitan volcanic area, have been performed using stratigraphical, volcanological …

The Agnano–Monte Spina tephra (AMST), dated at 4100 years BP by 40Ar/39Ar and 14C
AMS techniques, is the product of the highest-magnitude eruption in the Campi Flegrei …

The Campi Flegrei caldera is a complex structure in which resurgence occurs through a
simple shearing mechanism. The most uplifted block inside the caldera is the La Starza …

New geochronological, geochemical, and Sr-isotopic data on volcanics erupted before the
Campanian Ignimbrite (CI, 37 ka) and the Neapolitan Yellow Tuff (NYT, 12 ka) caldera …

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 …

The Tyrrhenian margin of central Italy has undergone Plio‐Quaternary extension,
develo** NW‐SE normal faults and NE‐SW faults. The NE‐SW faults decrease in …