Estudio preliminar sobre las facies volcaníclásticas de la Formación Zamoranos (Trías Subbético)
In some outcrops o f the Trias o f facies Keuper in the Central Subbetic Zone has been defined the Zamorano Formation, dated as Norian. In this formation is possible to identify conglomerates with pebbles of different nature, between them, the volcanogenetic ones. These last are present as porphyrit...
| Autores: | , |
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| Tipo de documento: | artigo |
| Data de publicação: | 1993 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositório: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | espanhol |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/14034 |
| Acesso em linha: | http://hdl.handle.net/10272/14034 |
| Access Level: | Acceso aberto |
| Palavra-chave: | Subbetic Triassic Norian Volcaniclastic facies Basalt |
| Resumo: | In some outcrops o f the Trias o f facies Keuper in the Central Subbetic Zone has been defined the Zamorano Formation, dated as Norian. In this formation is possible to identify conglomerates with pebbles of different nature, between them, the volcanogenetic ones. These last are present as porphyritic basaltic and glasses fragments. These volcaniclastic rocks have been interpreted as the result of a pre-or Norian volcanic activity in the south Iberian Triassic shelf |
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