Mareuil Anticline
id:
mareuil-anticline-276-17412988
title:
Mareuil Anticline
text:
The Mareuil Anticline, also called Mareuil-Meyssac Anticline, is a structural high within the sedimentary sequence of the northeastern Aquitaine Basin. The northwest-southeast trending anticline was caused by tectonic movements probably starting in the Upper Cretaceous.
brand slug:
wiki
category slug:
encyclopedia
description:
original url:
https://en.wikipedia.org/wiki/Mareuil_Anticline
date created:
date modified:
2023-12-18T06:56:20Z
main entity:
{"identifier":"Q1894744","url":"https://www.wikidata.org/entity/Q1894744"}
image:
fields total:
13
integrity:
13