Geochemical evidence for mixing between fluids exsolved at different depths in the magmatic system of Mt Etna (Italy)

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• 作者：Antonio Paonita^a ; ^{a.paonita@pa.ingv.it} ; Antonio Caracausi^a ; Giada Iacono-Marziano^b ; Mauro Martelli^a ; Andrea Rizzo^a
• 刊名：Geochimica et Cosmochimica Acta
• 出版年：2012
• 出版时间：1 May, 2012
• 年：2012
• 卷：84
• 期：Complete
• 页码：380-394
• 全文大小：1251 K

文摘

A 4-year geochemical survey of some fumaroles at the Voragine summit crater of Mt Etna was performed in combination with synchronous monitoring of peripheral gas emissions at the base of the volcano. This was the first geochemical study at Mt Etna to have included the abundances of Ar, He, and C isotopes. Once the effects of postmagmatic shallow processes were identified and quantitatively removed, the He-Ar-CO₂ systematics of the Voragine crater fumaroles and peripheral gas emissions described the same degassing path. Combining the carbon-isotope composition with information about noble gases provided evidence that the crater fumaroles are fed from a two-endmember mixture composed of a deep member coming from pressures between 200 and 400 MPa (depending on time), and a shallower one exsolved at ?30 MPa. Similar mixing processes probably also occur in gases from peripheral vents. The simultaneous assessment of ¦Ä¹³C_CO2 and He/Ar values of crater fumaroles over time has identified simple changes in the mixing proportion between the two endmembers and, moreover, periods during which the exsolution pressure of the deep fluid increased. These periods seem to be linked to pre-eruptive phases of the volcano. The identified open-system degassing processes are indicative of efficient bubble-melt decoupling at depth, whereas the mixing process requires a convective transfer of the deeply exsolved fluids toward shallower levels of magma where further vapor is exsolved. In agreement with the most recent geophysical and petrological data from Mt Etna, these observations allow inferences about a deep portion of the plumbing system (5 to 12 km b.s.l.), comprising sill-like reservoirs connected by small vertical structures, and a main reservoir at 2-3 km b.s.l. that is probably fluxed by magmatic volatiles.