scispace - formally typeset
F

Franco Tassi

Researcher at University of Florence

Publications -  228
Citations -  5159

Franco Tassi is an academic researcher from University of Florence. The author has contributed to research in topics: Volcano & Hydrothermal circulation. The author has an hindex of 38, co-authored 212 publications receiving 4343 citations. Previous affiliations of Franco Tassi include UniFi & National Research Council.

Papers
More filters
Journal ArticleDOI

Geochemistry of Quaternary travertines in the region north of Rome (Italy): structural, hydrologic and paleoclimatic implications

TL;DR: In this paper, the origin and transport of spring waters from which travertines precipitate are elucidated by chemical and isotopic studies of the travertine and associated thermal springs and gas vents.
Journal ArticleDOI

Fluid geochemistry of hydrothermal systems in the Arica-Parinacota, Tarapacá and Antofagasta regions (northern Chile)

TL;DR: In this article, the chemical and isotopic composition of water and gas thermal discharges from six hydrothermal systems in the Tarapaca and Antofagasta regions (northern Chile): Surire, Puchuldiza-Tuja, Pampa Lirima and Torta de Tocorcupi, to determine the chemical-physical conditions at the fluid source.
Journal ArticleDOI

Geochemical modeling of CO2 storage in deep reservoirs: The Weyburn Project (Canada) case study

TL;DR: In this article, the authors used the available dataset (bulk mineralogy of the reservoir, gas-cap composition and selected pre- and post-CO 2 injection water samples) provided by the International Energy Agency Weyburn CO 2 Monitoring & Storage Project (WEASP) to reconstruct the pre-injection reservoir chemical composition (including pH and the boundary conditions at 62°C and 15MPa).
Journal ArticleDOI

January 2002 volcano‐tectonic eruption of Nyiragongo volcano, Democratic Republic of Congo

TL;DR: In this article, the presence of three different phases during the Nyiragongo volcano's 2002 eruption is confirmed by new 238U and 232Th series radioactive disequilibria data, which show that the volcano is likely to change in the future, trending toward more common occurrence of flank eruptions.
Journal ArticleDOI

Water and gas chemistry at Lake Kivu (DRC): Geochemical evidence of vertical and horizontal heterogeneities in a multibasin structure

TL;DR: In this paper, water and dissolved gases collected along vertical profiles in the five basins (main, Kabuno Bay, Kalehe, Ishungu, and Bukavu) forming the 485 m deep Lake Kivu (Democratic Republic of the Congo) were analyzed to provide a geochemical conceptual model of the several processes controlling lake chemistry.