The central-western Mediterranean area is a key region for understanding the complex
interaction between igneous activity and tectonics. In this review, the specific geochemical …

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 …

A chronological reconstruction of the explosive activity of the south Italian volcanoes over
the past 80 ka is proposed from the geochemical study of marine tephra, interbedded in …

The central-western Mediterranean is one of the most important areas on Earth for studying
subduction-related potassic and ultrapotassic magmatism. In the circum-Tyrrhenian area …

The palynostratigraphic record from Lago Grande di Monticchio (S. Italy) is presented. An
independent sedimentation-rate-based chronology provides an age of 101,530 calendar …

Similar resurgent blocks occur in caldera depressions at the islands of Pantelleria and
Ischia. The two blocks, which are tilted, show similar deformation patterns and similar …

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 …

The volcanic island of Ischia is located on the Tyrrhenian margin of Central Italy,
characterized by Plio-Quaternary NW–SE-and NE–SW-trending extensional fractures. Ischia …