Dabie-Sulu orogeny
id:
dabie-sulu-orogeny-248-219658
title:
Dabie-Sulu orogeny
text:
The Dabie-Sulu orogeny also termed Qinling-Dabie-Sulu or Dabie Shan-Sulu was a mountain building event in the Triassic from 240 to 220 million years ago caused by the collision of the North China and South China cratons. It extends 2000 kilometers from the Tanlu fault zone between Shanghai and Wuhan in modern-day China to the Qaidam basin north of the Tibetan Plateau.
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Dabie-Sulu_orogeny
date created:
date modified:
2022-04-10T11:47:35Z
main entity:
{"identifier":"Q85755489","url":"https://www.wikidata.org/entity/Q85755489"}
image:
fields total:
13
integrity:
13