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...
Збережено в:
| Автори: | , , |
|---|---|
| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Asociación Argentina de Sedimentología
2025-12-01
|
| Серія: | Latin American Journal of Sedimentology and Basin Analysis |
| Предмети: | |
| Онлайн доступ: | https://lajsba.sedimentologia.org.ar/lajsba/article/view/267 |
| Теги: |
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|