Petrology of deep sea basalt near Hawaii

Clicks: 3
ID: 292621
1965
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 #3,885 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
Abstract
Dredge samples collected from the submarine part of the east rift zone of Kilauea Volcano consist of glassy, tholeiitic pillow basalts containing vesicles whose volume and size decrease systematically with depth. Basalt dredged from seamounts near the Island of Hawaii is weathered, and the large volume of vesicles indicates that the seamounts have submerged as much as 1,700 m since their lava was extruded. Close chemical similarity between the glassy crust of submarine pillows and subaerial lava of the same rift zone indicates that exchange does not take place between sea water and deep sea basalt at the time of eruption. There is no evidence that spilite forms at the time of eruption.
Reference Key
openalex_W2328806222 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors James G. Moore
Journal american journal of science
Year 1965
DOI
10.2475/ajs.263.1.40
URL
Keywords Keywords not found

Citations

No citations found. To add a citation, contact the admin at info@scimatic.org

No comments yet. Be the first to comment on this article.