Skip to main content

Main menu

  • Home
  • Content
    • Current
    • Archive
    • Special Volumes and Special Issue
  • Subscriptions
    • Subscribers
    • FAQ
    • Terms & Conditions for use of AJS Online
  • Instructions to Authors
    • Focus and paper options
    • Submit your manuscript
  • Site Features
    • Alerts
    • Feedback
    • Usage Statistics
    • RSS
  • About Us
    • Editorial Board
    • The Journal

User menu

  • Register
  • Subscribe
  • My alerts
  • Log in
  • My Cart

Search

  • Advanced search
American Journal of Science
  • Register
  • Subscribe
  • My alerts
  • Log in
  • My Cart
American Journal of Science

Advanced Search

  • Home
  • Content
    • Current
    • Archive
    • Special Volumes and Special Issue
  • Subscriptions
    • Subscribers
    • FAQ
    • Terms & Conditions for use of AJS Online
  • Instructions to Authors
    • Focus and paper options
    • Submit your manuscript
  • Site Features
    • Alerts
    • Feedback
    • Usage Statistics
    • RSS
  • About Us
    • Editorial Board
    • The Journal
  • Follow ajs on Twitter
  • Visit ajs on Facebook
  • Follow ajs on Instagram
OtherArticles

Phase relationships in the system NaAlSiO 4 -SiO 2 -H 2 O to 35 kilobars pressure

A. L. Boettcher and P. J. Wyllie
American Journal of Science October 1969, 267 (8) 875-909; DOI: https://doi.org/10.2475/ajs.267.8.875
A. L. Boettcher
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
P. J. Wyllie
  • Find this author on Google Scholar
  • Find this author on PubMed
  • Search for this author on this site
  • Article
  • References
  • Info & Metrics
  • PDF
Loading

Abstract

Phase relationships in the system are first presented on P-T projections of three different composition joins. Crystalline phases encountered include albite, analcite, coesite, jadeite, nepheline, and quartz. Vapor-saturated melting curves proceed with negative dP/dT slopes to invariant points of pressures between 10 and 13 kb. Together with chemographic methods of Schreinemakers and experimental data for the system NaAlSiO 4 -SiO 2 , univariant and invariant equilibria for the ternary system are presented on P-T projection. Isobaric polythermal diagrams, constructed on the basis of the melting relationships and solubility data illustrate the primary fields for the crystalline phases and disclose that critical phenomena will intervene only for compositions rich in SiO 2 .

This article requires a subscription to view the full text. If you have a subscription you may use the login form below to view the article. Access to this article can also be purchased.

Log in using your username and password

Forgot your user name or password?

Purchase access

You may purchase access to this article. This will require you to create an account if you don't already have one.
PreviousNext
Back to top

In this issue

American Journal of Science
Vol. 267, Issue 8
1 Oct 1969
  • Table of Contents
  • Table of Contents (PDF)
  • Index by author
Download PDF
Article Alerts
Sign In to Email Alerts with your Email Address
Email Article

Thank you for your interest in spreading the word on American Journal of Science.

NOTE: We only request your email address so that the person you are recommending the page to knows that you wanted them to see it, and that it is not junk mail. We do not capture any email address.

Enter multiple addresses on separate lines or separate them with commas.
Phase relationships in the system NaAlSiO 4 -SiO 2 -H 2 O to 35 kilobars pressure
(Your Name) has sent you a message from American Journal of Science
(Your Name) thought you would like to see the American Journal of Science web site.
CAPTCHA
This question is for testing whether or not you are a human visitor and to prevent automated spam submissions.
8 + 3 =
Solve this simple math problem and enter the result. E.g. for 1+3, enter 4.
Citation Tools
Phase relationships in the system NaAlSiO 4 -SiO 2 -H 2 O to 35 kilobars pressure
A. L. Boettcher, P. J. Wyllie
American Journal of Science Oct 1969, 267 (8) 875-909; DOI: 10.2475/ajs.267.8.875

Citation Manager Formats

  • BibTeX
  • Bookends
  • EasyBib
  • EndNote (tagged)
  • EndNote 8 (xml)
  • Medlars
  • Mendeley
  • Papers
  • RefWorks Tagged
  • Ref Manager
  • RIS
  • Zotero
Share
Phase relationships in the system NaAlSiO 4 -SiO 2 -H 2 O to 35 kilobars pressure
A. L. Boettcher, P. J. Wyllie
American Journal of Science Oct 1969, 267 (8) 875-909; DOI: 10.2475/ajs.267.8.875
Reddit logo Twitter logo Facebook logo Mendeley logo
  • Tweet Widget
  • Facebook Like
  • Google Plus One

Jump to section

  • Article
  • Info & Metrics
  • References
  • PDF

Related Articles

  • No related articles found.
  • Google Scholar

Cited By...

  • Phase equilibria in NaAlSiO4-KAlSiO4-SiO2-H2O at 100 MPa pressure: equilibrium leucite composition and the enigma of primary analcime in blairmorites revisited
  • Phase Relations Involving Hydrous Silicate Melts, Aqueous Fluids, and Minerals
  • Mineral solubility and hydrous melting relations in the deep earth: Analysis of some binary A H2O system pressure-temperature-composition topologies
  • The role of water in the synthesis of glaucophane
  • Kosmochlor and chromian jadeite aggregates from the Myanmar jadeitite area
  • New way to map old sutures using deformed alkaline rocks and carbonatites
  • EXPERIMENTAL STUDY OF THE SYSTEM DIOPSIDE ALBITE NEPHELINE AT P(H2O) = P(TOTAL) = 2 AND 10 KBAR AND AT P(TOTAL) = 28 KBAR
  • Experimental approach to constrain second critical end points in fluid/silicate systems: Near-solidus fluids and melts in the system albite-H2O
  • Google Scholar

More in this TOC Section

  • Timing and Nd-Hf isotopic mapping of early Mesozoic granitoids in the Qinling Orogen, central China: Implication for architecture, nature and processes of the orogen
  • India in the Nuna to Gondwana supercontinent cycles: Clues from the north Indian and Marwar Blocks
  • Unravelling the P-T-t history of three high-grade metamorphic events in the Epupa Complex, NW Namibia: Implications for the Paleoproterozoic to Mesoproterozoic evolution of the Congo Craton
Show more Articles

Similar Articles

Navigate

  • Current Issue
  • Archive

More Information

  • RSS

Other Services

  • About Us

© 2023 American Journal of Science

Powered by HighWire