Toco orogeny
id:
toco-orogeny-251-10584621
title:
Toco orogeny
text:
The Toco orogeny was a mountain building affecting the rocks of northern Chile and northwestern Argentina during the Late Carboniferous and Permian. In 1991, researchers Bahlburg and Breitkurz noted that Chilean rocks had a 100 million lull magmatic and metamorphic "lull" from the Silurian to the Carboniferous. They defined the Toco orogeny as the period when active margin conditions returned in the region.
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Toco_orogeny
date created:
date modified:
2022-02-08T07:00:17Z
main entity:
{"identifier":"Q85809892","url":"https://www.wikidata.org/entity/Q85809892"}
image:
fields total:
13
integrity:
13