Tectonic-palaeoenvironmental forcing of clay-mineral assemblages in nonmarine settings: the Oligocene-Miocene As Pontes Basin (Spain)
| Contribuinte(s) |
Universitat de Barcelona |
|---|---|
| Resumo |
Two small, alluvial-lacustrine subbasins developed during the early restraining overstep stages of the Oligocene-Miocene As Pontes strike-slip Basin (NW Spain). Later, the basin evolved into a restraining bend stage and an alluvial-swamp-dominated depositional framework developed. The palaeobiological record demonstrates that the Oligocene-Miocene palaeoclimate in NW Spain was subtropical, warm and humid to subhumid. |
| Identificador | |
| Idioma(s) |
eng |
| Publicador |
Elsevier B.V. |
| Direitos |
(c) Elsevier B.V., 2003 info:eu-repo/semantics/openAccess |
| Palavras-Chave | #Sediments fluvials #Oligocè #Miocè #Espanya #River sediments #Oligocene #Miocene #Spain |
| Tipo |
info:eu-repo/semantics/article info:eu-repo/semantics/acceptedVersion |
