Origin of the Black Peak Quartz Diorite, Northern Cascades, Washington

Clicks: 3
ID: 304995
1964
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 #434 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
Geologic and petrologic investigations of the quartz diorite and surrounding rocks indicate that this plutonic body was formed through recrystallization and local mobilization of the older Skagit Gneiss. Modal analyses of the Skagit Gneiss-Black Peak Quartz Diorite complex are tabulated, and percent distribution diagrams are shown for minerals, oxides, and Si cation.
Reference Key
openalex_W2317715245 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors J. B. Adams
Journal american journal of science
Year 1964
DOI
10.2475/ajs.262.3.290
URL
https://ajs.scholasticahq.com/article/59057.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.