Quartz solution reaction: 400°-500°C, 1000 bars-Reference-Cited by-同舟云学术

Quartz solution reaction: 400°-500°C, 1000 bars

Published:1967-08-15 Issue:16 Volume:72 Page:4253-4257
ISSN:0148-0227
Container-title:Journal of Geophysical Research
language:en
Short-container-title:J. Geophys. Res.

Author:

Sommerfeld R. A.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jz/v072/i016/JZ072i016p04253/JZ072i016p04253.pdf

Reference23 articles.

1. The solubility of quartz in supercritical water;Anderson;Am. J. Sci.,1965

2. Chemical nature of silica carried by steam;Brady;J. Phys. Chem.,1953

3. Mechanism of ‘solution’ of quartz in pure water at elevated temperatures and pressures;Frederickson;Am. Mineralogist,1954

4. The system NaAlSi2O6-H2O-argon: Total pressure and water pressure in metamorphism;Greenwood;J. Geophys. Res.,1961

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1. Thermodynamic properties and revised Helgeson-Kirkham-Flowers equations of state parameters of the hydrated and dehydrated monomeric silica species at t = 0.01–600oC, P = 1–3000 bars, ρH2O = 0.35–1.1 g cm−3, and I = 0 m;Applied Geochemistry;2024-11

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