Effect of paleomorphology on facies distribution of the Campania Ignimbrite in the northern Campania Plain, southern Italy

Ruberti, Daniela; Vigliotti, Marco; Rolandi, Roberto; Lascio, Massimo Di

doi:10.1016/b978-0-12-816454-9.00009-2

Cited by 10 publications

(13 citation statements)

References 23 publications

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“…The data from this work were compared with Ruberti et al (2020), who proposed contour maps of the lower and the upper surfaces of the CI for the northwestern sector of the proximalmedial area, based on 1,000 lithostratigraphic logs from boreholes. The extrapolated thicknesses from their maps were .…”

Section: Extracaldera Volumementioning

confidence: 99%

“…This difference is included in the 6.6 km 3 of the total volume error and uncertainties here presented. The data proposed by Ruberti et al (2020) were not inserted in the isopach map reported in this work to avoid error propagation due to data coming from contour maps rather than deposit thickness measurements. However, a greater thickness in the Volturno Plain compared to this work could be considered, as proposed by Ruberti et al (2020).…”

Section: Extracaldera Volumementioning

confidence: 99%

“…The data proposed by Ruberti et al (2020) were not inserted in the isopach map reported in this work to avoid error propagation due to data coming from contour maps rather than deposit thickness measurements. However, a greater thickness in the Volturno Plain compared to this work could be considered, as proposed by Ruberti et al (2020). The error and uncertainties associated with our volume estimate of the terrestrial CI ignimbrite deposits (68.2 ± 6.6 km 3 ) are less than 10% (Online Supplementary Material), a good precision considering that many published estimates of eruption volume may be barely more precise than one order of magnitude (Mason et al, 2004).…”

Section: Extracaldera Volumementioning

confidence: 99%

See 2 more Smart Citations

The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors

et al. 2020

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Section: Extracaldera Volumementioning

confidence: 99%

Section: Extracaldera Volumementioning

confidence: 99%

Section: Extracaldera Volumementioning

confidence: 99%

See 1 more Smart Citation

The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors

et al. 2020

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“…In particular, Campania Grey Tuff (CGT) deposition, originated by the Campi Flegrei caldera 39 ka eruption, sealed the marine-transitional environments that characterized the Campania plain at that time, and since 39 ky B.P. most of the coastal plain became emersed [31].…”

Section: Geological Settingmentioning

confidence: 99%

The Holocene Evolution of the Volturno Coastal Plain (Northern Campania, Southern Italy): Implications for the Understanding of Subsidence Patterns

Buffardi

Barbato²,

Vigliotti

et al. 2021

Water

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In the Mediterranean area, several alluvial coastal plains, developed after the Holocene transgression, are affected by subsidence. The Volturno alluvial-coastal plain, along the eastern Tyrrhenian Sea (southern Italy) is characterized by subsidence rates determined through InSAR data analysis and ranging between 0 and <−20 mm/yr in an area of about 750 kmq across the Volturno River. Inside this area, the pattern of subsidence shows sites with apparently anomalous localized subsidence. To understand the driving mechanisms of this process, a lithostratigraphic reconstruction was provided focusing on the spatial distribution of the horizons considered weak by a geotechnical point of view; then, the subsidence map was overlain spatially with geological data in a Geographic Information System (GIS) environment. The spatial analysis highlighted the major ground deformation occurring within the outer boundary of the incised paleo-valley, corresponding to the Holocene alluvial/transitional filling that overlies a compaction-free Pleistocene basement. Inside this general trend, differential compaction was detected corresponding to the thick occurrence of clay and peat deposits, suggesting that the subsidence rate registered in the plain are due in part to the consolidation of primary settlements of soft and compressible soils that characterize the subsoil of these areas, and in large part to the secondary consolidation settlements.

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Section: Extracaldera Volumementioning

confidence: 99%

Magnitude of the 39.8 ka Campanian Ignimbrite, Italy: insights from an ignimbrite isopach map

Silleni¹,

Giordano²,

Isaia³

et al. 2020

Preprint

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Effect of paleomorphology on facies distribution of the Campania Ignimbrite in the northern Campania Plain, southern Italy

Cited by 10 publications

References 23 publications

The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors

The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors

The Holocene Evolution of the Volturno Coastal Plain (Northern Campania, Southern Italy): Implications for the Understanding of Subsidence Patterns

Magnitude of the 39.8 ka Campanian Ignimbrite, Italy: insights from an ignimbrite isopach map

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