Colangüil Batholith
id:
colang-il-batholith-258-12709341
title:
Colangüil Batholith
text:
The Colangüil Batholith is a group of plutons in western Argentina between the latitudes of 29 and 31° S. The plutons of the batholith were emplaced and cooled in the Late Paleozoic and the Triassic. Runs in a north–south direction. The plutons of the batholith are intruded into volcanic rocks produced by the same plutons plus some earlier deformed basement. The most common rocks in the batholith are granodiorite, granite and leucogranite. The batholith contains also a dyke swarm of north–south
brand slug:
wiki
category slug:
encyclopedia
description:
Group of plutons in Argentina
original url:
https://en.wikipedia.org/wiki/Colang%C3%BCil_Batholith
date created:
date modified:
2024-03-15T09:42:02Z
main entity:
{"identifier":"Q28162990","url":"https://www.wikidata.org/entity/Q28162990"}
image:
fields total:
13
integrity:
14