Abstract
Eocene and Oligocene terrestrial sediments of the "Complexo de Benfica", near Lisbon, display different facies associations and two main infill sequences. They are separated by an unconformity. Depositional systems, controls and chronological boundaries are discussed.
Original language | Spanish |
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Pages (from-to) | 91-94 |
Number of pages | 4 |
Journal | Geogaceta |
Volume | 29 |
Publication status | Published - 2001 |
Keywords
- Eocene
- Oligocene
- sequences
- lower Tagus Basin