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Transpressive Tectonics Evidence in the Epicentral Area of the Modern Earthquake in Constantine Area of Algerian Eastern Tell Atlas: New Insights from Rhumel Valley

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Geotectonics Aims and scope

Abstract

The neotectonic processes are crucial for identification of active faults in a seismic unstable area. The Aїn Smara active fault runs along the Middle Rhumel Valley located in Constantine area of Algerian Eastern Tell Atlas mountain chain and it emerges in the south‒western part of the epicentral zone of the earthquake occurred on October 27, 1985 (Mw = 5.8) within a corridor displaying morphological features and deformed Pliocene‒Quaternary layers, which are the consequence of transpressive tectonic regime. In our study the morpho-tectonic and structural research supported by the fieldwork, was performed. The thick fault gouge indicating simple shear deformation, fault breccias and minor faults affecting the Pliocene limestone and Quaternary alluvial terraces, were found. The active fault splits into northern and southern segments. The northern segment corresponds to the El Aria Fault that ruptured during the earthquake in 1985 and the southern segment with the studied Aĭn Smara Fault. Our research showed the significant extent of the active fault and including its parameters for improved seismic hazard assessment of the Constantine area.

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ACKNOWLEDGMENTS

We acknowledge the General Directorate of Scientific Research and Technological Development (MERS/DGRSDT) (Algiers, Algeria), the National Centre of Research Applied for Earthquake Engineering (CGS) (Algiers, Algeria) and Geology Department belongs to Institute of Architecture and Earth Sciences of the University of Ferhat Abbes 1-Sétif (UFAS-1) (Sétif, Algeria) for the support of our research.

We are sincerely grateful to Christoph Grützner (Friedrich Schiller University, Jena Germany), Maouche Said (Astronomy Research Center Astrophysics and Geophysics, Algiers, Algeria), Benfedda Amar (Center of Research Applied for Earthquake Engineering, Algiers, Algeria) for their constructive discussions. We warmly thank our colleague Kheiri Ahmed (Center of Research Applied for Earthquake Engineering, Constantine, Algeria) for consultations. We are thankful to anonymous reviewers for useful comments and extend our gratitude to editor M.N. Shoupletsova (Geological Institute of Russian Academy of Sciences, Moscow, Russia) for careful editing.

Funding

This work was supported by Center of Research Applied for Earthquake Engineering (CGS) (Algiers, Algeria) as part of Research project.

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Aourari, S., Machane, D., Guemache, M. et al. Transpressive Tectonics Evidence in the Epicentral Area of the Modern Earthquake in Constantine Area of Algerian Eastern Tell Atlas: New Insights from Rhumel Valley. Geotecton. (2024). https://doi.org/10.1134/S0016852124700067

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