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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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carbon
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Macedonia
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geochemistry (1)
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igneous rocks
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volcanic rocks
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pyroclastics
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ignimbrite (1)
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Indian Ocean
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Arabian Sea
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Gulf of Oman (1)
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Invertebrata
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isotopes
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stable isotopes
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Mediterranean region (1)
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Wavelet analysis of δ 18 O and δ 13 C time-series from an Holocene speleothem record from Corchia Cave (central Italy): insights for the recurrence of dry-wet periods in the Central Mediterranean
An Oldest Dryas glacier expansion on Mount Pelister (Former Yugoslavian Republic of Macedonia) according to 10 Be cosmogenic dating
New findings of the Campanian Ignimbrite ash within slope deposits of the Treska valley (former Yugoslav Republic of Macedonia)
Duration and dynamics of the best orbital analogue to the present interglacial
A GIS-based approach for estimating volcaniclastic flow susceptibility: a case study from Sorrentina Peninsula (Campania Region)
New insights on the Holocene marine transgression in the Bahía Camarones (Chubut, Argentina)
Stalagmite evidence for the precise timing of North Atlantic cold events during the early last glacial
Late Holocene drought responsible for the collapse of Old World civilizations is recorded in an Italian cave flowstone
Volcaniclastic debris flows generated in drainage basins of the Apennine mountains of southern Campania in response to pyroclastic fall deposition from four Holocene eruptions of Somma-Vesuvius: Avellino (3.8 ka), A.D. 79, A.D. 472, and A.D. 1631. These syneruptive debris flows are lithologically homogeneous and contain more than 90% of material from the parental eruption. They differ from inter-eruptive debris flows recognized in the area, which contain mixed lithologies of juvenile material (i.e., volcanic material from different eruptions). Diffuse rill erosion generated fines-rich volcaniclastic flows (mudflows), whereas partial saturation of coarse ash and lapilli generated coarser-grained debris flows. Lithofacies analysis shows that debris flows predominate versus hyperconcentrated flows and normal stream-flow deposits. Debris-flow deposits are massive, matrix supported, and have a gravelly-sandy texture. Large blocks are scarce due to their absence in the pyroclastic source material. Lithofacies association indicates that volcaniclastic debris-flow deposits aggraded rapidly by superimposition of different surges that spontaneously developed within the flow. Bulk-flow density ranges from 1840 to 2260 kg/m 3 (mean 2035 ± 207 kg/m 3 ). Geological data supported some considerations of hazard assessment in the study area and indicate that the syneruptive volcaniclastic flows stopped distally on active alluvial fans.