Edge Rewrite
restyle Source code View original
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

Jump to content

Basement high

Edit links
From Wikipedia, the free encyclopedia
Cross section of the Weald in England. A basement high (the Hampshire-Dieppe High) can be seen in the centre-left.

In geology, a basement high is a portion of the basement in a sedimentary basin that is higher than its surroundings.[1] Commonly, basement highs are hidden by the sedimentary fill of the basin. Usually basement highs are elongated features of tectonic origin.[2]

References

[edit]
  1. ↑ David C. P. Peacock and Graham J. Banks (24 January 2022). "Evolution of the geological structure and mechanical properties due to the collision of multiple basement topographic highs in a forearc accretionary wedge: insights from numerical simulations".
  2. ↑ Ayumu Miyakawa, Atsushi Noda & Hiroaki Koge (11 March 2020). "Progress in Earth and Planetary Science volume 9, Article number: 1".


Retrieved from "https://en.wikipedia.org/w/index.php?title=Basement_high&oldid=1312481843"