Deep crustal hot zone
id:
deep-crustal-hot-zone-233-12897205
title:
Deep crustal hot zone
text:
The Deep Crustal Hot Zone (DCHZ), or just deep hot zone, is a zone in the lower crust where hot mantle material intrudes. In a volcanic arc setting, hot, molten material from the mantle may intrude into the lower crust. This hot material generates a new, more evolved melt in this area of the crust, which may collect and migrate upwards towards the upper crust. Here, it would collect in a magma chamber and later erupt. The upper crust consists mainly of evolved, intermediate to silicic magmatic r
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Deep_crustal_hot_zone
date created:
date modified:
2024-03-12T20:48:37Z
main entity:
{"identifier":"Q48999869","url":"https://www.wikidata.org/entity/Q48999869"}
image:
fields total:
13
integrity:
13