Chemical and isotopic signatures of the basement rocks from the Campi Flegrei geothermal field (Naples, southern Italy): inferences about the origin and evolution of its hydrothermal fluids-Reference-Cited by-同舟云学术

Chemical and isotopic signatures of the basement rocks from the Campi Flegrei geothermal field (Naples, southern Italy): inferences about the origin and evolution of its hydrothermal fluids

Published:1997-03 Issue:1-2 Volume:76 Page:63-82
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Caprarelli Graziella,Tsutsumi Makoto,Turi Bruno

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference41 articles.

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2. Isotopic study of the origin of sulfur and carbon in Solfatara fumaroles, Campi Flegrei caldera;Allard;J. Volcanol. Geotherm. Res.,1991

3. Geochemical temperatures of the thermal waters of Phlegrean Fields (Naples, Italy);Antrodicchia;Geotherm. Res. Counc. Trans.,1985

4. Magmatic fluid discharging to the surface from the Osorezan geothermal system, northern Honshu, Japan;Aoki,1991

5. The Phlegrean Fields: Magma evolution within a shallow chamber;Armienti;J. Volcanol. Geotherm. Res.,1983

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