1. High-resolution imaging of the faults bounding the Guadalentín Valley (SE Iberian Peninsula): The UnriDDLE Project
- Author
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Perea, Héctor, Herrero-Barbero, Paula, Li, Hongqiang, Carbonell, Ramón, Molins-Vigatà, J., Alcalde, Juan, Álvarez-Gómez, Jose A., Berriolópez Berriolópez Llamosas, Maria, de Pro Diáz, Y., Dufour, D, García-Mayordomo, Julian, Granja, Jose Luis, Insua-Arévalo, Juan M., Martí, David, Martín-Banda, R., Masana, Eulàlia, Ollé, M., Pascual-Sanchez, E., Portela, J. J., Rivera, Jhonathan, Sánchez-Roldán, José Luis, Staller, Alejandra, Rameez, S., Perea, Héctor, Herrero-Barbero, Paula, Li, Hongqiang, Carbonell, Ramón, Molins-Vigatà, J., Alcalde, Juan, Álvarez-Gómez, Jose A., Berriolópez Berriolópez Llamosas, Maria, de Pro Diáz, Y., Dufour, D, García-Mayordomo, Julian, Granja, Jose Luis, Insua-Arévalo, Juan M., Martí, David, Martín-Banda, R., Masana, Eulàlia, Ollé, M., Pascual-Sanchez, E., Portela, J. J., Rivera, Jhonathan, Sánchez-Roldán, José Luis, Staller, Alejandra, and Rameez, S.
- Abstract
The Guadalentin Depression is bordered by an active left-lateral strike-slip fracture system, which serves as the corresponding tectonic boundary. This depression is a significant elongated Plio-Quaternary basin located within the deformation corridor of the Eastern Betic Shear Zone (EBSZ), trending in a NE-SW direction. Stretching for about 100 km, the western margin of the basin is characterized by a prominent mountain front mainly controlled by the Alhama de Murcia fault. Along with other major faults such as the Carrascoy and the Palomares faults, and some secondary related minor fractures, the whole system may absorb part of the deformation related to the convergence between Iberia and North Africa (4-5 mm/yr). As a result, the system show a moderate seismic activity; however some large and damaging events have occurred in the area. Notably, the most recent significant earthquake was a 5.1 magnitude event in 2011, which occurred near the town of Lorca and was associated to the Alhama de Murcia fault. In addition, active tectonics and paleoseismological studies carried out in all the system have shown that faults have produce large earthquakes during the Holocene and late Quaternary. Even though, there is still a lack of knowledge about the deep structure of the faults. In order to address this shortcoming, we have acquired high-resolution seismic reflection transects, one across the Palomares Fault, three across the Alhama de Murcia fault, and one across the Carrascoy fault. The seismic data was acquired using a mini-Vib system, which provided sufficient energy to produce seismic sections reaching depths of over 2 km. The resulting high-resolution seismic reflection images are allowing to unveil the deep structure and geometry of the region, providing valuable insights into the upper Neogene deformation history. Additionally, these images have revealed fracture branches in the subsurface, contributing to a better understanding of the region's geological charact
- Published
- 2023