Relative dating of peneplains and sediments in the Lake Albert rift area

Clicks: 1
ID: 305780
1965
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 #7,269 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
Rifting caused deposition of a sequence in the Lake Albert rift spanning the periods Miocene to lower Pleistocene in the now provisionally accepted stratigraphical column. It shows no major breaks of sedimentation. As the initial age of the P-II cycle is thought to be considerably pre-Miocene, that cycle may span part of Mesozoic time as well as the early Tertiary.
Reference Key
openalex_W2168696550 Use this key to autocite in the manuscript while using SciMatic Manuscript Manager or Thesis Manager
Authors Achilles Gautier
Journal american journal of science
Year 1965
DOI
10.2475/ajs.263.6.537
URL
https://ajs.scholasticahq.com/article/61418.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.