Coastal salina evaporites of the Triassic-Liassic boundary in the Iberian Peninsula
The evaporite unit (the Lécera Formation), which was formed at the Triassic-Liassic boundary in the Aragonian Branch of the Iberian Chain, was studied at the 01 Alacón borehole (Alacón village, Teruel province), where it is mainly constituted by a thick (.
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2004 |
| País: | España |
| Institución: | Universitat Autònoma de Barcelona |
| Repositorio: | Dipòsit Digital de Documents de la UAB |
| Idioma: | inglés |
| OAI Identifier: | oai:ddd.uab.cat:86066 |
| Acceso en línea: | https://ddd.uab.cat/record/86066 https://dx.doi.org/urn:doi:10.1344/105.000001421 |
| Access Level: | acceso abierto |
| Palabra clave: | Evaporites Anhydrite Salina Triassic-Liassic boundary Iberian Chain |
| Sumario: | The evaporite unit (the Lécera Formation), which was formed at the Triassic-Liassic boundary in the Aragonian Branch of the Iberian Chain, was studied at the 01 Alacón borehole (Alacón village, Teruel province), where it is mainly constituted by a thick (. |
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