Chonide orogeny
id:
chonide-orogeny-262-14298011
title:
Chonide orogeny
text:
The Chonide orogeny was a mountain building event in the Triassic, preserved in coastal accretionary complexes in southwestern Chile. The Chonos Metamorphic Complex, Madre de Dios Accretionary Complex and Diego de Almagro Complex all crop out west of the South Patagonian Batholith. Rocks in the Chonos Metamorphic Complex include turbidites as well as meta-chert and mafic schist. Some researchers propose that during the Permian, the supercontinent Gondwana moved rapidly northward leading to the f
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wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Chonide_orogeny
date created:
date modified:
2022-02-07T03:33:55Z
main entity:
{"identifier":"Q85752208","url":"https://www.wikidata.org/entity/Q85752208"}
image:
fields total:
13
integrity:
13