Earth-prints repository, logo   DSpace

About DSpace Software
|earth-prints home page | roma library | bologna library | catania library | milano library | napoli library | palermo library
Please use this identifier to cite or link to this item:

Authors: Rizzo, A. L.*
Caracausi, A.*
Chavagnac, V.*
Nomikou, P.*
Polymenakou, P. N.*
Mandalakis, M.*
Kotoulas, G.*
Magoulas, A.*
Castillo, A.*
Lampridou, D.*
Title: Kolumbo submarine volcano (Greece): An active window into the Aegean subduction system
Title of journal: Nature Scientific Reports
Series/Report no.: /6 (2016)
Issue Date: 17-Jun-2016
DOI: 10.1038/srep28013
Keywords: Kolumbo
submarine volcano
volcanic gases
hydrothermal system
volcanic arc
crustal contamination
Abstract: Submarine volcanism represents ~80% of the volcanic activity on Earth and is an important source of mantle-derived gases. These gases are of basic importance for the comprehension of mantle characteristics in areas where subaerial volcanism is missing or strongly modified by the presence of crustal/atmospheric components. Though, the study of submarine volcanism remains a challenge due to their hazardousness and sea-depth. Here, we report 3He/4He measurements in CO2–dominated gases discharged at 500 m below sea level from the high-temperature (~220 °C) hydrothermal system of the Kolumbo submarine volcano (Greece), located 7 km northeast off Santorini Island in the central part of the Hellenic Volcanic Arc (HVA). We highlight that the mantle below Kolumbo and Santorini has a 3He/4He signature of at least 7.0 Ra (being Ra the 3He/4He ratio of atmospheric He equal to 1.39×10−6), 3 Ra units higher than actually known for gases-rocks from Santorini. This ratio is also the highest measured across the HVA and is indicative of the direct degassing of a Mid-Ocean-Ridge- Basalts (MORB)-like mantle through lithospheric faults. We finally highlight that the degassing of high-temperature fluids with a MORB-like 3He/4He ratio corroborates a vigorous outgassing of mantlederived volatiles with potential hazard at the Kolumbo submarine volcano.
Appears in Collections:04.07.08. Volcanic arcs
04.07.06. Subduction related processes
05.02.01. Geochemical data
04.08.01. Gases
03.04.06. Hydrothermal systems
04.07.07. Tectonics
04.07.02. Geodynamics
Papers Published / Papers in press

Files in This Item:

File SizeFormatVisibility
Rizzo et al., 2016.pdf1.56 MBAdobe PDFNot available View/Open

This item is licensed under a Creative Commons License
Creative Commons

Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.

Share this record




Stumble it!



Valid XHTML 1.0! ICT Support, development & maintenance are provided by CINECA. Powered on DSpace Software. CINECA