Solubility and speciation of C–O–H fluids in andesitic melt at T=1100–1300°C and P=200 and 500MPa-Reference-Cited by-同舟云学术

Solubility and speciation of C–O–H fluids in andesitic melt at T=1100–1300°C and P=200 and 500MPa

Published:2006-05 Issue:1-3 Volume:229 Page:125-143
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Botcharnikov R.E.,Behrens H.,Holtz F.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference75 articles.

1. Quantification of water speciation in silicate glasses by IR spectroscopy — in situ vs. quench technique;Behrens;Phase Transit.,2003

2. Quantification of H2O contents in silicate glasses using IR spectroscopy—a calibration based on hydrous glasses analyzed by Karl–Fischer titration;Behrens;Glass Sci. Technol.,2003

3. CO2 solubility in dacitic melts equilibrated with H2O–CO2 fluids — implications for modelling the solubility of CO2 in silicic melts;Behrens;Geochim. Cosmochim. Acta,2004

4. H2O diffusion in dacitic and andesitic melts;Behrens;Geochim. Cosmochim. Acta,2004

5. Determination of the molar absorption coefficient for the infrared absorption band of CO2 in rhyolitic glasses;Behrens;Am. Mineral.,2004

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