AVO Logo
Site Map | FAQ |
Alaska Volcano Observatory
Introduction | Reference Search | Glossary 
You are here: Home > Library > Hydroxyl, Cl, and F partitioning between high-silica rhyolitic melts-apatite-fluid(s) at 50-200 MPa and 700-1000 degrees C

HYDROXYL, CL, AND F PARTITIONING BETWEEN HIGH-SILICA RHYOLITIC MELTS-APATITE-FLUID(S) AT 50-200 MPA AND 700-1000 DEGREES C
Webster, J.D., Goldoff, B.A., Flesch, R.N., Nadeau, P.A., and Silbert, Z.W., 2017, Hydroxyl, Cl, and F partitioning between high-silica rhyolitic melts-apatite-fluid(s) at 50-200 MPa and 700-1000 degrees C: American Mineralogist, v. 102, n. 1, p. 61-74.
Contact AVO Privacy Accessibility Information Quality FOIA
URL: avo.alaska.edu/downloads/reference.php
Page modified: February 16, 2017 16:07
Contact Information: AVO Web Team

twitter @alaska_avo
facebook alaska.avo
email 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.