The system Mg 2 SiO 4 -Mg 2 GeO 4

Clicks: 2
ID: 297094
1956
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
Emerging

Ranked #6,730 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
Mg ~2~ SiO ~4~ and Mg ~2~ GeO ~4~ form a continuous series of solid solutions. The melting behavior is of the Roozeboom type I. Similarity of melting point and latent heat of melting are indicative of the close thermochemical and structural relationship between the two end members. Attempts to prepare the spinel polymorph of Mg ~2~ GeO ~4~ described by Goldschmidt were unsuccessful. It seems likely that the spinel modification is monotropic and is formed only under specialized and restricted conditions.
Reference Key
openalex_W2145880062 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors A. E. Ringwood
Journal american journal of science
Year 1956
DOI
10.2475/ajs.254.11.707
URL
https://ajs.scholasticahq.com/article/58580.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.