6533b823fe1ef96bd127f733

RESEARCH PRODUCT

Anomalous Behavior of Zirconium and Hafnium in Volcanic Fumarolic Fluids

P. CensiP. ZuddasA. CaracausiF. SortinoM. CangemiD. PiazzeseV. CensiE. Falcone

subject

GeophysicsGeneral Earth and Planetary SciencesZr/Hf ratio volcanic fumarolesSettore CHIM/01 - Chimica AnaliticaSettore GEO/08 - Geochimica E Vulcanologia

description

The Zirconium and Hafnium concentrations in worldwide fumaroles fed by magmatic fluids reveal that the Zr/Hf ratio is inversely related to the temperature of emission. Lower Zr/Hf ratio values below the chondritic signature are found in fluids having the highest temperature while super-chondritic Zr/Hf ratio values are found in lower temperatures. Sub-chondritic values of the Zr/Hf ratio may be related to larger volatility of Hf-chloride gas species with respect to Zr-Cl gas species, while super-chondritic ratios may correspond to fluid-rock processes resulting from cooling of uprising magmatic fluids. We propose that subchondritic Zr/Hf ratio values in fumaroles associated with high temperature may be an appropriate marker of fast magmatic rising representing a new sensitive tool for volcanic risks strategies.

https://doi.org/10.1029/2021gl094674