Tuhua orogeny
id:
tuhua-orogeny-322-15021031
title:
Tuhua orogeny
text:
The Tuhua orogeny was a regional orogeny between 370 and 330 million years ago, now preserved in the Fiordland region of New Zealand. Early Paleozoic rocks such as Ordovician greywacke, slate and paragneiss in the Buller terrane, weakly metamorphosed greenschist and sub-greenschist rocks, Cambrian mafic volcanics, Ordovician limestone and Silurian clastic rocks were all deformed and metamorphosed. In addition, between 380 and 250 million years ago, metasediments reached amphibolite grade in the
brand slug:
wiki
category slug:
encyclopedia
description:
Mountain-building process in New Zealand
original url:
https://en.wikipedia.org/wiki/Tuhua_orogeny
date created:
date modified:
2024-01-23T17:32:58Z
main entity:
{"identifier":"Q56278694","url":"https://www.wikidata.org/entity/Q56278694"}
image:
fields total:
13
integrity:
14