Alaska Volcano Observatory - Solubility and fluid-melt partitioning of H 2 O and Cl in andesitic magmas as a function of pressure between 50 and 500MPa

You are here: Home > Library > Solubility and fluid-melt partitioning of H 2 O and Cl in andesitic magmas as a function of pressure between 50 and 500MPa

SOLUBILITY AND FLUID-MELT PARTITIONING OF H 2 O AND CL IN ANDESITIC MAGMAS AS A FUNCTION OF PRESSURE BETWEEN 50 AND 500MPA

Botcharnikov, R. E., Holtz, F., and Behrens, H., 2015, Solubility and fluid-melt partitioning of H 2 O and Cl in andesitic magmas as a function of pressure between 50 and 500MPa: Chemical Geology, v. 418, p. 117-131.

Contact AVO Privacy Accessibility Information Quality FOIA

URL: www.avo.alaska.edu/downloads/reference.php
Page modified: June 22, 2022 08:39
Contact Information: AVO Web Team

@alaska_avo

alaska.avo

Receive volcano updates by email: USGS VNS

This website is supported by the U.S. Geological Survey under Cooperative Agreement Grant G19AC00060 and G19AC00171.

Mention of trade names or commercial products does not constitute their endorsement by the U.S. Geological Survey.