Ring dike

From Wikipedia, the free encyclopedia

Jump to: navigation, search

A ring dike or ring dyke in geology refers to an intrusive igneous body. Their chemistry, petrology and field appearance precisely match those of dikes or sill, but their concentric or radial geometric distribution around a centre of volcanic activity indicates their sub-volcanic origins.

One of the best exposed and studied is the Loch Bà ring dike, Isle of Mull, Scotland.

[edit] See also

pl:Dajki pierścieniowe
Views
Personal tools

Toolbox