The gas/steam ratio as indicator of heat transfer at the Solfatara fumaroles, Phlegraean Fields (Italy)-Reference-Cited by-同舟云学术

The gas/steam ratio as indicator of heat transfer at the Solfatara fumaroles, Phlegraean Fields (Italy)

Published:1984-06 Issue:2 Volume:47 Page:295-302
ISSN:0258-8900
Container-title:Bulletin Volcanologique
language:en
Short-container-title:Bull Volcanol

Author:

Cioni R.,Corazza E.,Marini L.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/BF01961560.pdf

Reference20 articles.

1. Armienti, P., Barberi, F., Bizouard, H., Clocchiatti, R., Innocenti, F., Metrich, N., Rosi, M., andSbrana, A., 1982,The Phlegraean Fields: Magma Evolution within a Shallow Magma Chamber. InM.F. Sheridan andF. Barberi (Editors),Explosive Volcanism. J. Volc. Geotherm. Res.,16.

2. Barin, I., andKnacke, O., 1973,Thermochemical properties of inorganic substances. Springer-Verlag, Berlin, 921 pp.

3. Cioni, R., andCorazza, E., 1981,Medium Temperature Fumarolic Gas Sampling. Bull. Volcanol.,44-1, p. 23–29.

4. —— ——, andPescia, A., 1980,Sampling and Analysis of Medium — High Temperature Fumarolic Gases. Workshop on Volcanic Gases, Gif-sur-Yvette.

5. --, --, andMagro, G., 1983,Gases at Solfatara (Italy); Surveillance Implications. Presented at IUGG XVIII General Assembly, Hamburg.

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