Southern Oklahoma Aulacogen
id:
southern-oklahoma-aulacogen-285-597830
title:
Southern Oklahoma Aulacogen
text:
The Southern Oklahoma Aulacogen is a failed rift, or failed rift arm (aulacogen), of the triple junction that became the Iapetus Ocean spreading ridges. It is a significant geological feature in the Western and Southern United States. It formed sometime in the early to mid Cambrian Period and spans the Wichita Mountains, Taovayan Valley, Anadarko Basin, and Hardeman Basin in Southwestern Oklahoma. The Southern Oklahoma Aulacogen is primarily composed of basaltic dikes, gabbros, and units of gran
brand slug:
wiki
category slug:
encyclopedia
description:
Failed rift in the western and southern US of the triple junction that became the Iapetus Ocean
original url:
https://en.wikipedia.org/wiki/Southern_Oklahoma_Aulacogen
date created:
date modified:
2023-04-04T00:27:10Z
main entity:
{"identifier":"Q25021345","url":"https://www.wikidata.org/entity/Q25021345"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/en/0/03/Ussoamap.png","width":620,"height":449}
fields total:
13
integrity:
15