Kibaran orogeny
id:
kibaran-orogeny-273-6906596
title:
Kibaran orogeny
text:
The Kibaran orogeny is a term that has been used for a series of orogenic events, in what is now Africa, that began in the Mesoproterozoic, around 1400 Ma and continued until around 1000 Ma when the supercontinent Rodinia was assembled.
The term "Kibaran" has often been used for any orogenic rocks formed during this very extended period.
Recently, it has been proposed that the term should be used in a much narrower sense for an event around 1375 Ma and a region in the southeast of the Democratic
brand slug:
wiki
category slug:
encyclopedia
description:
Mountain building event in what is now Africa
original url:
https://en.wikipedia.org/wiki/Kibaran_orogeny
date created:
date modified:
2023-11-21T20:14:06Z
main entity:
{"identifier":"Q6403956","url":"https://www.wikidata.org/entity/Q6403956"}
image:
fields total:
13
integrity:
14