Hunter-Bowen orogeny
id:
hunter-bowen-orogeny-290-14446718
title:
Hunter-Bowen orogeny
text:
The Hunter-Bowen Orogeny was a significant arc accretion event in the Permian and Triassic periods affecting approximately 2,500 km of the Australian continental margin. The Hunter-Bowen Orogeny occurred in two main phases: The first being Permian accretion of passive-marginal Devonian- and Carboniferous-age sediments, occurring in the Hunter region, as well as the mid-west region of what is now New South Wales, followed by rifting, back-arc volcanism. The later Permian to Triassic event consist
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Hunter-Bowen_orogeny
date created:
date modified:
2024-03-29T01:30:47Z
main entity:
{"identifier":"Q5944166","url":"https://www.wikidata.org/entity/Q5944166"}
image:
fields total:
13
integrity:
13