Phase relations in the system MgO-SiO 2 -H 2 O at high temperatures and pressures

Clicks: 1
ID: 293599
1966
Free PDF
Article Quality & Performance Metrics
Overall Quality
Not rated
Combines reader engagement with the AI quality analysis. This article has not been analysed, so there is no overall score — reader engagement is measured and shown alongside.
AI Quality Assessment
Not analyzed
Readership in this journal

Ranked #6,663 of 8,486 articles by views in american journal of science

Most read Least read

Bar heights use a square-root scale. Only the 120 most-read articles are drawn; the journal has 8,486 in total.

Mint this article as an NFT
Not yet minted

Create a permanent, verifiable on-chain record of this article on the Scimatic Network. The NFT is held in your Journament account, and you can withdraw it to your own wallet at any time.

5 SUSD one-off · no wallet required
Sign in to mint
Abstract
Phase assemblages were determined at water pressures up to 30 kb and temperatures up to 900 degrees C for the following four equilibria: (1) serpentine+brucite=forsterite+vapor; (2) serpentine=forsterite+talc+vapor; (3) forsterite+talc=enstatite+vapor; and (4) talc=enstatite+quartz (or coesite)+vapor. The dP/dT= for equilibria 1, 2, and 4 above 10 kb, and is negative for 3 above 5 kb. The data show that water pressures can be increased to at least 30 kb without the formation of a primary serpentine magma.
Reference Key
openalex_W4253931865 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors S. Kitahara, S. Takenouchi, G. C. Kennedy
Journal american journal of science
Year 1966
DOI
10.2475/ajs.264.3.223
URL
https://ajs.scholasticahq.com/article/59122.pdf
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

Comments

No comments yet. Be the first to comment on this article.