Fumarolic minerals: an overview of active European volcanoes

Tonci Balic Zunic; Anna Garavelli; Sveinn Peter Jakobsson; Kristjan Jonasson; Athanasios Katerinopoulos; Konstantinos Kyriakopoulos; Pasquale Acquafredda

Fumarolic minerals: an overview of active European volcanoes

Tonci Balic Zunic, Anna Garavelli, Sveinn Peter Jakobsson, Kristjan Jonasson, Athanasios Katerinopoulos, Konstantinos Kyriakopoulos, Pasquale Acquafredda

Geology

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Abstract

The fumarolic mineralogy of the Icelandic active volcanoes, the Tyrrhenian volcanic belt (Italy) and the Aegean active arc (Greece) is investigated, and literature data surveyed in order to define the characteristics of the European fumarolic systems. They show broad diversity of mineral associations, with Vesuvius and Vulcano being also among the world localities richest in mineral species. Volcanic systems, which show recession over a longer period, show fumarolic development from the hightemperature alkaline halide/sulphate, calcic sulphate or sulphidic parageneses, synchronous with or immediately following the eruptions, through mediumtemperature ammonium minerals, metal chlorides, or fluoride associations to the late low-temperature paragenesis dominated by sulphur, gypsum, alunogen, and other hydrous sulphates. The situation can be different in the systems that are not recessing but show fluctuations in activity, illustrated by the example of Vulcano where the high-temperature association appears intermittently. A full survey of the mineral
groups and species is given in respect to their importance and appearance in fumarolic associations.

Original language	English
Title of host publication	Updates in Volcanology - From Volcano Modelling to Volcano Geology
Editors	Karoly Nemeth
Number of pages	56
Publisher	InTechOpen
Publication date	2016
Pages	267-322
Chapter	11
Publication status	Published - 2016

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Fumarolic Minerals An Overview of Active EuropeanFinal published version, 51.1 MBLicence: CC BY

http://www.intechopen.com/books/updates-in-volcanology-from-volcano-modelling-to-volcano-geology/fumarolic-minerals-an-overview-of-active-european-volcanoesLicence: CC BY

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Balic Zunic, T., Garavelli, A., Jakobsson, S. P., Jonasson, K., Katerinopoulos, A., Kyriakopoulos, K., & Acquafredda, P. (2016). Fumarolic minerals: an overview of active European volcanoes. In K. Nemeth (Ed.), Updates in Volcanology - From Volcano Modelling to Volcano Geology (pp. 267-322). InTechOpen. http://www.intechopen.com/books/updates-in-volcanology-from-volcano-modelling-to-volcano-geology/fumarolic-minerals-an-overview-of-active-european-volcanoes

Balic Zunic, T, Garavelli, A, Jakobsson, SP, Jonasson, K, Katerinopoulos, A, Kyriakopoulos, K & Acquafredda, P 2016, Fumarolic minerals: an overview of active European volcanoes. in K Nemeth (ed.), Updates in Volcanology - From Volcano Modelling to Volcano Geology. InTechOpen, pp. 267-322. <http://www.intechopen.com/books/updates-in-volcanology-from-volcano-modelling-to-volcano-geology/fumarolic-minerals-an-overview-of-active-european-volcanoes>

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abstract = "The fumarolic mineralogy of the Icelandic active volcanoes, the Tyrrhenian volcanic belt (Italy) and the Aegean active arc (Greece) is investigated, and literature data surveyed in order to define the characteristics of the European fumarolic systems. They show broad diversity of mineral associations, with Vesuvius and Vulcano being also among the world localities richest in mineral species. Volcanic systems, which show recession over a longer period, show fumarolic development from the hightemperature alkaline halide/sulphate, calcic sulphate or sulphidic parageneses, synchronous with or immediately following the eruptions, through mediumtemperature ammonium minerals, metal chlorides, or fluoride associations to the late low-temperature paragenesis dominated by sulphur, gypsum, alunogen, and other hydrous sulphates. The situation can be different in the systems that are not recessing but show fluctuations in activity, illustrated by the example of Vulcano where the high-temperature association appears intermittently. A full survey of the mineralgroups and species is given in respect to their importance and appearance in fumarolic associations.",

author = "{Balic Zunic}, Tonci and Anna Garavelli and Jakobsson, {Sveinn Peter} and Kristjan Jonasson and Athanasios Katerinopoulos and Konstantinos Kyriakopoulos and Pasquale Acquafredda",

year = "2016",

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T1 - Fumarolic minerals

T2 - an overview of active European volcanoes

AU - Balic Zunic, Tonci

AU - Garavelli, Anna

AU - Jakobsson, Sveinn Peter

AU - Jonasson, Kristjan

AU - Katerinopoulos, Athanasios

AU - Kyriakopoulos, Konstantinos

AU - Acquafredda, Pasquale

PY - 2016

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N2 - The fumarolic mineralogy of the Icelandic active volcanoes, the Tyrrhenian volcanic belt (Italy) and the Aegean active arc (Greece) is investigated, and literature data surveyed in order to define the characteristics of the European fumarolic systems. They show broad diversity of mineral associations, with Vesuvius and Vulcano being also among the world localities richest in mineral species. Volcanic systems, which show recession over a longer period, show fumarolic development from the hightemperature alkaline halide/sulphate, calcic sulphate or sulphidic parageneses, synchronous with or immediately following the eruptions, through mediumtemperature ammonium minerals, metal chlorides, or fluoride associations to the late low-temperature paragenesis dominated by sulphur, gypsum, alunogen, and other hydrous sulphates. The situation can be different in the systems that are not recessing but show fluctuations in activity, illustrated by the example of Vulcano where the high-temperature association appears intermittently. A full survey of the mineralgroups and species is given in respect to their importance and appearance in fumarolic associations.

AB - The fumarolic mineralogy of the Icelandic active volcanoes, the Tyrrhenian volcanic belt (Italy) and the Aegean active arc (Greece) is investigated, and literature data surveyed in order to define the characteristics of the European fumarolic systems. They show broad diversity of mineral associations, with Vesuvius and Vulcano being also among the world localities richest in mineral species. Volcanic systems, which show recession over a longer period, show fumarolic development from the hightemperature alkaline halide/sulphate, calcic sulphate or sulphidic parageneses, synchronous with or immediately following the eruptions, through mediumtemperature ammonium minerals, metal chlorides, or fluoride associations to the late low-temperature paragenesis dominated by sulphur, gypsum, alunogen, and other hydrous sulphates. The situation can be different in the systems that are not recessing but show fluctuations in activity, illustrated by the example of Vulcano where the high-temperature association appears intermittently. A full survey of the mineralgroups and species is given in respect to their importance and appearance in fumarolic associations.

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EP - 322

BT - Updates in Volcanology - From Volcano Modelling to Volcano Geology

A2 - Nemeth, Karoly

PB - InTechOpen

ER -

Fumarolic minerals: an overview of active European volcanoes

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