Código QR

Provenance and depositional processes of extrabasinal (siliciclastic) and intrabasinal (carbonate) particles of the Tithonian–Berriasian Vaca Muerta–Quintuco System (Neuquén Basin, Argentina)

During the Early Jurassic–Early Cretaceous, between 32° and 40° S latitude, a steeply dipping active subduction zone along the western margin of Gondwana led to the development of a magmatic arc and a large back-arc depression known as the Neuquén Basin. A thick record of Tithonian–Berriasian organ...

Descrición completa

Gardado en:
Detalles Bibliográficos
Principais autores: Luis Spalletti, Ernesto Schwarz, Gonzalo D. Veiga
Formato: Artigo
Idioma:Inglês
Publicado: Asociación Argentina de Sedimentología 2025-12-01
Series:Latin American Journal of Sedimentology and Basin Analysis
Assuntos:
Acceso en liña:https://lajsba.sedimentologia.org.ar/lajsba/article/view/267
Tags: Engadir etiqueta
Sen Etiquetas, Sexa o primeiro en etiquetar este rexistro!