Origin of albite in granitic rocks

Clicks: 1
ID: 302833
1961
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 #5,705 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
Albite in granites commonly occurs adjacent to K feldspar, either as rims on oligoclase or as small scattered grains. The albite was not derived either from adjacent K feldspar or from more calcic plagioclase and appears to have formed roughly synchronously with the K feldspar. Consequently, the albite appears to be a product of direct crystallization during the later stages of magmatic solidification.
Reference Key
openalex_W2333473615 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. J. W. Rogers
Journal american journal of science
Year 1961
DOI
10.2475/ajs.259.3.186
URL
https://ajs.scholasticahq.com/article/58858.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.