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Chapter
The Problem of Volcanic Unrest: The Campi Flegrei Case History
Campi Flegrei is one of the most densely populated active volcanic areas of the world. It consists of a complex structure with a multicollapse caldera and many postcaldera, explosive, mostly monogenetic vents....
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Article
Compositional variation in the 1983 and other recent Etnean lavas: Insights on the shallow feeding system
A systematic petrographic and chemical study of chronologically ordered lava samples collected during the 1983 Etna eruption, has shown minor fluctuating variations in crystallinity and chemistry, apparently c...
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Article
Foreword
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Article
Foreword
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Article
A model of the Phlegraean Fields magma chamber in the last 10,500 years
Volcanological and petrological data suggest that the Phlegraean Fields volcanic activity has been fed, at least in the last 10,500 years, by a not-refilled magma chamber where trachytic residual liquids were ...
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Article
Phlegraean Fields 1982–1984: Brief chronicle of a volcano emergency in a densely populated area
The essential features of the ongoing potential pre-eruptive crisis at the Phlegraean Fields begun in August 1982 are summarized and the main problems faced by scientists responsible of volcanic hazards evalua...
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Article
The evolution of latera caldera (central Italy) in the light of subsurface data
Subsurface geothermal exploration has considerably added to our knowledge of the Latera volcanic complex. A syenitic body is located about 2 km below the present-day surface; K-Ar data point a 0.9 Ma age. The ...
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Article
Compositional variations in the Campanian Ignimbrite, Italy: Hydrothermal modification or pre-eruptive fractionation? — A reply
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Article
Preface
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Article
The somma-vesuvius magma chamber: a petrological and volcanological approach
The volcanic history of Somma-Vesuvius indicates that salic products compatible with an origin by fractionation within a shallow magma chamber have been repeatedly erupted («Plinian» pumice deposits). The last...
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Article
Metamorphic carbonate ejecta from vesuvius plinian eruptions: Evidence of the occurrence of shallow magma chambers
Petrological, mineralogical and chemical data of 46 ejecta deriving from the sedimentary basement beneath Somma-Vesuvius volcano are reported. The ejecta samples were collected in pumice deposits formed during...
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Chapter and Conference Paper
The Evaluation of a Preliminary Geothermal Model for the Phlegraean Fields Volcanic Area (Italy)
The results of volcanological and petrochemical studies, MT surveys, passive seismic studies and a new gravity and magnetic interpretation relatively to the Phlegraean Fields area, Italy, are presented.
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Chapter and Conference Paper
Integrated Geothermal Reconnaissance of the Somma-Vesuvius System
The main results of the first phase of the geothermal exploration of Somma-Vesuvius active volcanic area (including geologic, volcanological, hydrogeological, hydrogeochemical, gravimetric, aeromagnetic, geoel...
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Article
Upper miocene submarine basalts from the western margin of the Red Sea (Secca Fawn-l hole, massawa channel)
Die Secca-Fawn-l-Bohrung, die 1968 von der Gulf Oil Company am westlichen Rand des südlichen Roten Meeres abgeteuft wurde, erreichte in 1400 m Tiefe eine Folge von jungmiozänen bis altpliozänen submarinen Basa...
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Article
The campanian ignimbrite: a major prehistoric eruption in the Neapolitan area (Italy)
A geological, chemical and petrographical study of the Campanian ignimbrite, a pyroclastic flow deposit erupted about 30,000 years ago on the Neapolitan area (Italy), is reported. The ignimbrite covered an are...
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Chapter and Conference Paper
The Afar Rift Junction
The Afar depression (Ethiopia and Gibuti area) is the site of the junction of three major rift zones: two oceanic (Red Sea and Gulf of Aden) and a continental one (East African rift). Approaching Afar some mod...
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Article
Editorial
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Editorial
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Editorial
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Article
Volcanological research in afar (L. R. Wager prize summary lecture)