The Large Explosive Activity of Mt. Etna as Recorded in Distal Tephrostratigraphy

被引：0

作者：

Sulpizio, Roberto ^{[1
,2
]}

Groppelli, Gianluca ^{[2
]}

Insinga, Donatella ^{[3
]}

Branca, Stefano ^{[4
]}

Del Carlo, Paola ^{[5
]}

Tamburrino, Stella ^{[3
]}

Zanchetta, Giovanni ^{[6
]}

机构：

[1] Dipartimento Sci Terra & Geoambientali, I-70125 Bari, Italy

[2] CNR, Ist Dinam Proc Ambientali, I-20133 Milan, Italy

[3] CNR, Ist Ambiente Marino & Costiero, I-80125 Naples, Italy

[4] Ist Nazl Geofis & Vulcanol, Sez Catania, I-95125 Catania, Italy

[5] Ist Nazl Geofis & Vulcanol, Sez Pisa, I-56126 Pisa, Italy

[6] Dipartimento Sci Terra, I-56126 Pisa, Italy

来源：

STRATI 2013 | 2014年

关键词：

Mount Etna; Tephrostratigraphy; Explosive eruptions; Mediterranean area; VOLCANIC ACTIVITY; MOUNT-ETNA; ERUPTION; TEPHROCHRONOLOGY; SEA;

D O I：

10.1007/978-3-319-04364-7_245

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

Mt. Etna is renowned for being the most active and highest volcano in Europe. Lava flows and weak explosive eruptions characterize its activity, but intermediate to large explosive eruptions have punctuated its eruptive history. Marine and lacustrine distal records are excellent archives for the recognition of past large explosive activity at Mt. Etna, as testified by the recognition of distal tephra layers of Pleistocene to Holocene age. These data are, to date, neither organised nor correlated to the proximal stratigraphic and chronological records. Here, we propose the reorganisation and correlation of the distal tephra layers from Mt. Etna in order to decipher the timings and frequency of its major explosive eruptions.

引用

页码：1281 / 1283

页数：3

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