INTRODUCTION
Italian Plio-Quaternary magmatism exhibits a very
wide petrological, geochemical and radiogenic-isotope variability, which makes
magma genesis and geodynamic significance difficult issues. A
large number of papers have been published on these rocks trying to
explain the petrogenesis and evolution of single volcanoes or
magmatic provinces. However, papers presenting a comprehensive review of
the data and hypotheses on the magmatism of the region as a whole are few,
if any. Synthesis of data at the local scale has definitely increased our
degree of understanding of volcanism at that scale, but it has not
resolved ambiguous issues such as the relationship among various magmatic
provinces, the significance of regional compositional variations, and the
geodynamic setting for this complex magmatism. The objective of this book
is to fill this gap by providing an overview of the most prominent
petrological and geochemical data and discussing currently held ideas on
the petrogenesis and geodynamic significance of Italian Plio-Quaternary
volcanic rocks. In summarising the intense debate on Italian magmatism, I
have tried to report on, as objectively as possible, all the most
significant ideas. The different weight given to the discussion of various
points of view depends only marginally on the author’s choice but is
mostly an effect of the very different amounts of factual constraints
which have been brought to supporting various hypotheses.
Fig 1. Italian Plio-Quaternary Magmatism By Angelo P. Book |
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