Cordón de Lila
id:
cord-n-de-lila-238-16768944
title:
Cordón de Lila
text:
Cordón de Lila is a mountain range of the Andes located in northern Chile, south of Salar de Atacama. Geologically it is made up of a batholith of Cambrian and Ordovician age. The rocks of Cordón de Lila are the result of pre-Andean magmatism that occurred during the Famatinian orogeny. The compositions of the plutonic rocks are granodiorite and monzogranite that are either metaluminous or marginally peraluminous. These rocks are remnants of the magmatism along the western rim of the Famatinian
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Cord%C3%B3n_de_Lila
date created:
date modified:
2023-04-16T15:07:33Z
main entity:
{"identifier":"Q104829976","url":"https://www.wikidata.org/entity/Q104829976"}
image:
fields total:
13
integrity:
13