
handle: 10272/18154
Este artículo trata las características sedimentológicas de la unidad inferior litoestratigráfica del Pérmico del borde noreste del Sistema Central. Se establecen tres grandes secuencias, las cuales dan como resultado un desarrollo cíclico de facies distales de abanico aluvial.
This paper deals with the sedimentological features of the Permian lowermost lithostratigraphic unit in the northeastern edge of the Spanish Central System. Three major sequences are established. They result in a ciclicity development of alluvial fan distal facies
Alluvial fam, Permian, Central System
Alluvial fam, Permian, Central System
| selected citations These citations are derived from selected sources. This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | 0 | |
| popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network. | Average | |
| influence This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically). | Average | |
| impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network. | Average |
