Deep hydrothermal circulation in a granite intrusion beneath Larderello geothermal area (Italy): constraints from mineralogy, fluid inclusions and stable isotopes-Reference-Cited by-同舟云学术

Deep hydrothermal circulation in a granite intrusion beneath Larderello geothermal area (Italy): constraints from mineralogy, fluid inclusions and stable isotopes

Published:2003-08 Issue:3-4 Volume:126 Page:243-262
ISSN:0377-0273
Container-title:Journal of Volcanology and Geothermal Research
language:en
Short-container-title:Journal of Volcanology and Geothermal Research

Author:

Boyce A.J,Fulignati P,Sbrana A

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference62 articles.

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3. Refinement of the evaluation of the role of CO2 in modifying estimates of pressure of epithermal mineralization;Barton;Econ. Geol.,1993

4. Deep structure, age and evolution of the Larderello–Travale geothermal field;Batini;Geotherm. Res. Counc. Trans.,1985

5. Fluid inclusions in minerals from the geothermal fields of Tuscany, Italy;Belkin;Geothermics,1985

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