refs 5, 6, 7, 8, 9, 10, 11, 12), investigation of the geochemical glass composition (e.g. refs 12 and 15), modelling of eruption dynamics and tephra dispersal (e.g. 3), relationship of the stratigraphic position of the CI tephra relative to palaeoclimatic (e.g. The yellow shaded area is the dispersal areal of the CI tephra within the 0.5 cm isopach of the simulated ash fallout model. (b) Geological sketch of the Campanian Ignimbrite (CI) pyroclastic deposits and isopach map of the CI Plinian fall (from ref.
refs 12 and 13), physical volcanology of proximal Plinian deposits (e.g. 3, 6 and references therein) with the location of the analysed samples of CI deposit for The age and stratigraphic position of the CI are important elements to the investigation of many chronostratigraphic problems in European volcanology, palaeoclimatology and archaeology.
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In this framework, the study of distal volcanic ash – ejected into atmosphere during large explosive eruptions and near-simultaneously deposited in diverse sedimentary environments up to thousands of kilometres from the source – has in the last several decades seen increased attention (e.g. Full realization of the potential of a marker tephra is a function of: (i) unequivocal correlations from site-to-site based on a host of parameters such as lithology, geochemistry, paleomagnetism, and approximate age; (ii) accurate knowledge of its dispersal area, and (iii) detailed assessment of stratigraphic events and processes in the sections where the tephra is found.
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