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Median Subbetic Outcrops

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The Toarcian Oceanic Anoxic Event in the South Iberian Palaeomargin

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Abstract

The Iznalloz (IZ) section is located in the km 13 of the Granada-Moreda railway scarpment (N 37° 23′ 24.4″; E 03° 29′ 19.5″), 3 km east of the village of Iznalloz (Granada Province, Figs. 3.1 and 4.1). The study section pertains to the Toarcian of the Zegrí Formation, and contains alternating marls and marly limestones in the lower part with nodular marly limestones (ammonitico rosso facies) in the upper part.

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Authors and Affiliations

  1. Departamento de Geología and CEACT, Universidad de Jaén, Jaén, Spain

    Matías Reolid, José Miguel Molina & Luis Miguel Nieto

  2. Departamento de Estratigrafía y Paleontología, Universidad de Granada, Granada, Spain

    Francisco Javier Rodríguez-Tovar

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  1. Matías Reolid
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  2. José Miguel Molina
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  3. Luis Miguel Nieto
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  4. Francisco Javier Rodríguez-Tovar
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Correspondence to Matías Reolid .

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Reolid, M., Molina, J.M., Nieto, L.M., Rodríguez-Tovar, F.J. (2018). Median Subbetic Outcrops. In: The Toarcian Oceanic Anoxic Event in the South Iberian Palaeomargin . SpringerBriefs in Earth Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-67211-3_4

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