Sleaford orogeny
id:
sleaford-orogeny-190-5905957
title:
Sleaford orogeny
text:
The Sleaford orogeny was an event in the assembly of the Gawler Craton, which now underlies the Eyre Peninsula in South Australia. Between 2.46 and 2.41 billion years ago in the Proterozoic, the Sleaford and Mulgathing complexes emplaced among the older 3.15 billion year old Archean Cooyerdoo Granite 2.82 billion year old Coolanie Gneiss with sedimentary, felsic and ultramafic igneous rocks. The overlapping Sleaford orogeny caused deformation and greenschist and granulite-grade metamorphism on t
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Sleaford_orogeny
date created:
date modified:
2022-04-26T21:38:58Z
main entity:
{"identifier":"Q85801570","url":"https://www.wikidata.org/entity/Q85801570"}
image:
fields total:
13
integrity:
13