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Geochemical indicators of possible ongoing volcanic unrest at Nisyros Island (Greece)
Author(s) -
Chiodini Giovanni,
Brombach Tatjana,
Caliro Stefano,
Cardellini Carlo,
Marini Luigi,
Dietrich Volker
Publication year - 2002
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2001gl014355
Subject(s) - fumarole , hydrothermal circulation , unrest , volcano , geology , caldera , geochemistry , earth science , seismology , politics , political science , law
Significant changes occurred in the chemistry of gases discharged from Nisyros fumaroles in the years, 1997–2001, following a strong seismic crisis. Increasing H 2 S/CO 2 ratios and decreasing CH 4 /CO 2 ratios are attributed to an increased contribution of magmatic fluids to the hydrothermal system. Some fumaroles showed concurrent increases in H 2 and CO contents implying increases in temperature and pressure in the upper parts of the hydrothermal system. These changes reinforce the possibility of an increased hazard of hydrothermal eruptions at present with respect to the '90's. Moreover, both the present events and the historical hydrothermal eruptions may represent precursory signals of a new period of volcanic unrest at Nisyros.