shear zone
geology
Quick Summary
A shear zone in geology is an area characterized by shear structures or closely spaced, parallel faults. These zones often act as pathways for underground solutions and are sites where ore deposits can form.1
In the context of plate tectonics, shear occurs when lithospheric plates slide past one another. These zones of shear link other plate boundaries and are known as transform faults.234
Summary created from Britannica articles
using AI.
AI can make mistakes, so verify using Britannica articles.
4 Britannica Sources
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.
