Geochemical monitoring of the 2002–2003 eruption at Stromboli volcano (Italy): precursory changes in the carbon and helium isotopic composition of fumarole gases and thermal waters

2005 ◽  
Vol 68 (2) ◽  
pp. 118-134 ◽  
Author(s):  
G. Capasso ◽  
M. L. Carapezza ◽  
C. Federico ◽  
S. Inguaggiato ◽  
A. Rizzo
2016 ◽  
Vol 16 (3) ◽  
pp. 113-123
Author(s):  
Vasilios Zarikas ◽  
K.E. Anagnostou ◽  
P. Avlakiotis ◽  
S. Kotsopoulo ◽  
C. Liolios ◽  
...  

1995 ◽  
pp. 61-64
Author(s):  
R. Bodmer ◽  
P. Bochsler ◽  
J. Geiss ◽  
R. Von Steiger ◽  
G. Gloeckler

1995 ◽  
Vol 72 (1-2) ◽  
pp. 61-64 ◽  
Author(s):  
R. Bodmer ◽  
P. Bochsler ◽  
J. Geiss ◽  
R. von Steiger ◽  
G. Gloeckler

2006 ◽  
Vol 40 (3) ◽  
pp. 245-252 ◽  
Author(s):  
E. FOURRE ◽  
P. JEAN-BAPTISTE ◽  
J.-L. CHARLOU ◽  
J. P. DONVAL ◽  
J. I. ISHIBASHI

Author(s):  
E. G. Kalacheva ◽  
Yu. A. Taran

Many active volcanoes of the Kuril Islands host hydrothermal systems. Their surface manifestations are represented by numerous thermal springs showing diverse chemical composition and physical-chemical parameters. Four main isotopic shifts relative to the local meteoric water line can be observed in the corresponding δD vs. δ18O diagrams. For the acid Cl-SO4 waters there is a clear mixing trend between meteoric water and volcanic vapor. The acid SO4waters demonstrate trends indicating kinetic fractionation at temperatures close to the boiling-point. Isotopic composition of the coastal springs tend to march the mixing line between meteoric and seawater. The δ18O-shift for deep thermal water is accounted to of isotopic exchange with host rock. The latitude effect revealed for meteoric waters also observed in the isotopic composition of the thermal waters.


2008 ◽  
Vol 43 (5) ◽  
pp. 429-453 ◽  
Author(s):  
B. G. Polyak ◽  
E. O. Dubinina ◽  
V. Yu. Lavrushin ◽  
A. L. Cheshko

2000 ◽  
Vol 177 (3-4) ◽  
pp. 273-285 ◽  
Author(s):  
Finlay M Stuart ◽  
Robert M Ellam ◽  
Paul J Harrop ◽  
J.Godfrey Fitton ◽  
Brian R Bell

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