Temporal evolution of a three component system: the island of Lipari (Aeolian Arc, southern Italy)

Crisci, Gino Mirocle; Rosa, R. De; Esperança, Sonia; Mazzuoli, R.; Sonnino, Maurizio

doi:10.1007/bf00301231

Cited by 127 publications

(125 citation statements)

References 36 publications

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“…As an alternative hypothesis, it has also been proposed that the Aeolian volcanism results from an asthenospheric uplift linked to the postsubduction extensional strain determined by the opening of the Tyrrhenian Sea (Wang et al, 1989;Crisci et al, 1991;Esperança et al, 1992). Crustal thinning and oceanic accretion have affected the Tyrrhenian area since the early-middle Miocene with an eastward migration.…”

Section: Introductionmentioning

confidence: 99%

“…HKCA-high-K alkaline series; SHO-shoshonitic series; KS-potassic series. Data, reported on water-free basis, are unpublished data and from Romano (1973); Keller (1980aKeller ( , 1980b; Lanzafame and Rossi (1984); Francalanci et al (1988Francalanci et al ( , 1989Francalanci et al ( , 1993aFrancalanci et al ( , 1993b; Bargossi et al (1989); Ellam et al (1989); Crisci et al (1991); Esperança et al (1992); Peccerillo and Wu (1992); Calanchi et al (1993Calanchi et al ( , 2002; Francalanci and Santo (1993); Peccerillo et al (1993); Ventura (1995);De Astis et al (1997, 2000; Del Moro et al (1998); Gertisser and Keller (2000); Gioncada et al (2003); Santo et al (2004).…”

Section: Introductionmentioning

confidence: 99%

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A west-east geochemical and isotopic traverse along the volcanism of the Aeolian Island arc, southern Tyrrhenian Sea, Italy: Inferences on mantle source processes

Francalanci¹,

Avanzinelli²,

Tommasini³

et al. 2007

Cenozoic Volcanism in the Mediterranean Area

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Section: Introductionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

A west-east geochemical and isotopic traverse along the volcanism of the Aeolian Island arc, southern Tyrrhenian Sea, Italy: Inferences on mantle source processes

Francalanci¹,

Avanzinelli²,

Tommasini³

et al. 2007

Cenozoic Volcanism in the Mediterranean Area

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“…After 23.5 ka, the activity yielded rhyolitic fall and surge deposits followed by the extrusion of lava domes (Mts. Guardia and Giardina; Crisci et al, 1991). In the same phase of Mts.…”

Section: Liparimentioning

confidence: 99%

“…Volcanic activity at Lipari started at around 220 ka (Crisci et al, 1991) with andesitic products on the western coast (Pichler, 1980). The activity of Mt.…”

Section: Liparimentioning

confidence: 99%

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High-resolution aeromagnetic anomaly map of the Vulcano-Lipari volcanic complex, Aeolian Islands, Italy

茂雄

正

Supper

et al. 2006

Bull. Geol. Surv. Japan

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Tephrochronological dating of varved interglacial lake deposits from Piànico‐Sèllere (Southern Alps, Italy) to around 400 ka

Brauer

Wulf

Mangili

et al. 2006

J Quaternary Science

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2006. Tephrochronological dating of varved interglacial lake deposits from Piànico-Sèllere (Southern Alps, Italy) to around 400 ka.ABSTRACT: The sediment record from the Piànico palaeolake in the southern Alps is continuously varved, spans more than 15 500 years, and represents a key archive for interglacial climate variability at seasonal resolution. The stratigraphic position of the Piànico Interglacial has been controversial in the past. The identification of two volcanic ash layers and their microscopic analysis provides distinct marker layers for tephrochronological dating of these interglacial deposits. In addition to micro-facies analyses reconstructing depositional processes of both tephra layers within the lake environment, their mineralogical and geochemical composition has been determined through major-element electron probe micro-analysis on glass shards. Comparison with published tephra data traced the volcanic source regions of the Piànico tephras to the Campanian volcanic complex of Roccamonfina (Italy) and probably the Puy de Sancy volcano in the French Massif Central. Available dating of near-vent deposits from the Roccamonfina volcano provides a robust tephrochronological anchor point at around 400 ka for the Piànico Interglacial. These deposits correlate with marine oxygen isotope stage (MIS) 11 and thus are younger than Early to Middle Pleistocene previously suggested by K/Ar dating and older than the last interglacial as inferred from macrofloral remains and the geological setting.

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Temporal evolution of a three component system: the island of Lipari (Aeolian Arc, southern Italy)

Cited by 127 publications

References 36 publications

A west-east geochemical and isotopic traverse along the volcanism of the Aeolian Island arc, southern Tyrrhenian Sea, Italy: Inferences on mantle source processes

A west-east geochemical and isotopic traverse along the volcanism of the Aeolian Island arc, southern Tyrrhenian Sea, Italy: Inferences on mantle source processes

High-resolution aeromagnetic anomaly map of the Vulcano-Lipari volcanic complex, Aeolian Islands, Italy

Tephrochronological dating of varved interglacial lake deposits from Piànico‐Sèllere (Southern Alps, Italy) to around 400 ka

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