Details

Autor(en) / Beteiligte

• Alfaro, P.
• Sánchez-Alzola, A.
• Martin-Rojas, I.
• García-Tortosa, F.J.
• Galindo-Zaldívar, J.
• Avilés, M.
• Garrido, A.C. López
• de Galdeano, C. Sanz
• Ruano, P.
• Martínez-Moreno, F.J.
• Pedrera, A.
• Lacy, M.C.
• Borque, M.J.
• Medina-Cascales, I.
• Gil, A.J.

Titel

Geodetic fault slip rates on active faults in the Baza sub-Basin (SE Spain): Insights for seismic hazard assessment

Ist Teil von

• Journal of geodynamics, 2021-03, Vol.144, p.101815, Article 101815

Ort / Verlag

Elsevier Ltd

Erscheinungsjahr

2021

Quelle

Alma/SFX Local Collection

Beschreibungen/Notizen

• •The Central Betic Cordillera (SE Spain) is dominated by NE-SW regional extension.•We obtain the first short-term slip rates for two active faults in the Baza sub-Basin.•Slip rate for the normal Baza Fault ranges between 0.3 ± 0.3 mm/yr and 1.3 ± 0.4 mm/yr.•Slip rate for the trike-slip Galera Fault is 0.5 ± 0.3 mm/yr.•The Baza Fault accommodates one-third of the regional extension. One of the most significant parameters for seismic hazard assessment analyses is the fault slip rate. The combination of both geological (long-term) and geodetic (short-term) data offers a more complete characterization of the seismic potential of active faults. Moreover, geodetic data are also a helpful tool for the analysis of geodynamic processes. In this work, we present the results of a local GPS network from the Baza sub-Basin (SE Spain). This network, which includes six sites, was established in 2008 and has been observed for seven years. For the first time, we obtain short-term slip rates for the two active faults in this area. For the normal Baza Fault, we estimate slip rates ranging between 0.3 ± 0.3 mm/yr and 1.3 ± 0.4 mm/yr. For the strike-slip Galera Fault, we quantify the slip rate as 0.5 ± 0.3 mm/yr. Our GPS study shows a discrepancy for the Baza Fault between the short-term slip rates and previously reported long-term rates. This discrepancy indicates that the fault could be presently in a period with a displacement rate higher than the mean of the magnitude 6 seismic cycle. Moreover, the velocity vectors that we obtained also show the regional tectonic significance of the Baza Fault, as this structure accommodates one-third of the regional extension of the Central Betic Cordillera. Our GPS-related slip rates form the basis for future seismic hazard analysis in this area. Our results have further implications, as they indicate that the Baza and Galera Faults are kinematically coherent and they divide the Baza sub-Basin into two tectonic blocks. This points to a likely physical link between the Baza and Galera Faults; hence, a potential complex rupture involving both faults should be considered in future seismic hazard assessment studies.