Structure and origin of an ultramafic pluton in the Klamath Mountains, California
Clicks: 1
ID: 296830
1964
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.
Reader Engagement
0.0
/100
1 views
0 readers
AI Quality Assessment
Not analyzed
Readership in this journal
Ranked #3,902 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 mintedCreate 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
Abstract
The geologic setting of the late Jurassic Trinity pluton and its structural relationship with country rock are discussed. Some detailed mineralogy and petrology, especially textures and structures in the ultramafic rocks, are presented, on the basis of which it is concluded that emplmplacement involved flowage and recrystallization of essentially crystalline material at temperatures ranging from 700 degrees C in the interior to less than 500 degrees C at contacts.\--H.C.W.S
Abstract Quality Issue:
This abstract appears to be incomplete or contains metadata (71 words).
Try re-searching for a better abstract.
| Reference Key |
openalex_W1969378533
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | Peter W. Lipman |
| Journal | american journal of science |
| Year | 1964 |
| DOI |
10.2475/ajs.262.2.199
|
| URL | |
| 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.