Description and occurrence of atoll phosphate rock in Micronesia
Clicks: 4
ID: 297076
1957
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
Steady Performance
0.9
/100
4 views
0 readers
AI Quality Assessment
Not analyzed
Readership in this journal
SteadyRanked #1,459 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
Formation of phosphate rock found below a surface layer of humus on Jemo and other islands of the Marshall group is belived to be recent and in some cases contemporary. It is concluded that calcium phosphate of guano is dissolved as it is washed through the acid humus by rain water and is then precipitated (as a brown cement in which apatite is a major constituent) on contact with the underlying limy sands.
| Reference Key |
openalex_W2319697366
Use this key to autocite in the manuscript while using
SciMatic Manuscript Manager or Thesis Manager
|
|---|---|
| Authors | F. Raymond Fosberg |
| Journal | american journal of science |
| Year | 1957 |
| DOI |
10.2475/ajs.255.8.584
|
| 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.