Descripción
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In the eastern Canary Islands: Gran Canaria, Fuerteventura and Lanzarote are located mio-pliocene marine deposits. These deposits consist in a reddish fossiliferous conglomerate and sandstones with structures and bioturbation, which are interpreted as belonging to a shallow environment. In some sites, these marine deposits appear below lava flows. In Salinas del Janubio (Lanzarote) are under basalts from T¿?as-Janubio Formation, dated about 6.6 Myr and 8.9 Myr. In the Barranco de Aju¿? (Fuerteventura) dated about 4.8 Myr and in the Barranco de Los Dolores and Tamaraceite (Gran Canaria) are associated with pillow lava flows dated as 4.1 Myr. | |
Internacional
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No |
Nombre congreso
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Congreso: IV Congress of Marine Sciences Publicación: Book of Abstracts |
Tipo de participación
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960 |
Lugar del congreso
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Las Palmas de Gran Canaria |
Revisores
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Si |
ISBN o ISSN
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84-697-0471-0 |
DOI
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Fecha inicio congreso
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11/06/2014 |
Fecha fin congreso
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13/06/2014 |
Desde la página
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203 |
Hasta la página
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203 |
Título de las actas
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Oral Comunications |