Tectono-Sedimentary Evolution of the Cenozoic Basins in the Eastern External Betic Zone (SE Spain)
Abstract
:1. Introduction
2. Background History
3. Geological Setting
4. Stratigraphic Framework
4.1. Murcia Sector (Cenozoic Pila-Carche Basin)
4.2. Alicante Sector (Cenozoic Alicante Trough and Agost Basin)
5. Tectono-Sedimentary Evolution of the Cenozoic Basins of the Eastern External Betic Zone
5.1. The Murcia Sector (Cenozoic Pila-Carche Basin)
- (i)
- The Upper Paleocene–Upper Eocene tectono-stratigraphic unit (Figure 8) shows, after an initial transgression, a progressive shallowing upward marine trend. During the Paleocene to Early Eocene, the sedimentation (Alberquilla, Garapacha, Pinoso-Rasa fms) reflects a slope environment that evolved during the Middle–Late Eocene to a carbonate platform environment (Miñano Fm). A main unconformity boundary in the Early Oligocene marks a stratigraphic gap also evidenced by a widespread paleokarst, pointing out an emersion of the basin.
- (ii)
- During the Oligocene (Murtas Fm), a transgression occurred with the development of marshy and beach lithofacies (Figure 8), followed by a new regressive depositional trend indicated by continental lacustrine and fluvial deposits during most of the Oligocene up to the Aquitanian.
- (iii)
- The Upper Burdigalian–Upper Serravallian tectono-stratigraphic unit (Pila-Carche Basin, Figure 9) shows a transgressive-regressive trend. The transgression, which began in the Late Burdigalian, reaching the Late Langhian (Congost Fm), results younger in some sectors of the basins because of the onlap arrangement of transgressive deposits on the previous deformed succession. The evolution begins with an internal platform environment sedimentation, while during the Early Langhian, a mixed carbonate and terrigenous supply indicates an external platform to upper slope environment.
- (iv)
- The Middle Tortonian tectono-stratigraphic unit (Pila-Carche Basin) shows a new transgressive-regressive cycle (Upper member of the Tap Fm). According to the sedimentological data, the depositional environment of this unit ranges between internal mixed (carbonate and siliciclastic) platform to external platform. Reworked Triassic clays and gypsum (olisthostromes) indicate a deposition on a slope realm. In this phase, the faulting reached the surface, generating thrusts and strike-slip faults and related features. The blocks between the faults were also folded and sometimes developed to form nappes.
5.2. Alicante Sector (Cenozoic Alicante Trough and Agost Basin)
6. Discussion and Conclusions
Author Contributions
Funding
Acknowledgments
Conflicts of Interest
References
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Martín-Martín, M.; Guerrera, F.; Tramontana, M. Tectono-Sedimentary Evolution of the Cenozoic Basins in the Eastern External Betic Zone (SE Spain). Geosciences 2020, 10, 394. https://doi.org/10.3390/geosciences10100394
Martín-Martín M, Guerrera F, Tramontana M. Tectono-Sedimentary Evolution of the Cenozoic Basins in the Eastern External Betic Zone (SE Spain). Geosciences. 2020; 10(10):394. https://doi.org/10.3390/geosciences10100394
Chicago/Turabian StyleMartín-Martín, Manuel, Francesco Guerrera, and Mario Tramontana. 2020. "Tectono-Sedimentary Evolution of the Cenozoic Basins in the Eastern External Betic Zone (SE Spain)" Geosciences 10, no. 10: 394. https://doi.org/10.3390/geosciences10100394