Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4688117 | Journal of Geodynamics | 2014 | 13 Pages |
Abstract
Moreover, the unit boundaries do not coincide with those of the familiar Exxon coastal aggradational curve, but rather with the local or regional tectonic activity. Consequently, the correlation of the unit boundaries with those of the Pliocene deposits of the eastern Betic basins remains difficult. According to the biostratigraphical data, the Pl-1, Pl-2, and Pl-3 units correspond to the Pliocene-I by Montenat (1990), while the Pl-4 unit may be equivalent to the Pliocene-II.
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Earth and Planetary Sciences
Earth-Surface Processes
Authors
Antonio Guerra-Merchán, Francisco Serrano, Rachid Hlila, Khalil El Kadiri, Carlos Sanz de Galdeano, Miguel Garcés,