Metadata
Author: ParaCrawl Corpus
Data
English[en]
It is interpreted that within the concave region, where the density contrast is negative, the graben accommodates some 3500-m thick sedimentary sequences that were deposited during an episode of crustal extension in Jurassic times.
Spanish[es]
Se interpreta que la región cóncava, donde el contraste en densidad es negativo, contiene el mayor espesor sedimentario sintectónico del Jurásico (~3500 m).