Abstract
The Djemila active fault is a NE–SW trending and NW-dipping reverse fault. Historical seismicity around this fault is weak to moderate. However, field observations allowed us to observe differential uplifts of quaternary alluvial terraces on the hanging and foot walls. We interpret this as a strong evidence of recent tectonic activity. The uplifted terraces suggests an uplift rate of 0.14 mm/years. Therefore, the seismic potential of this fault may be greater than may be suggested by the historical seismicity of the region.
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References
Anderson H, Jackson J (1988) Active tectonics of the Adriatic region. Geophys JR Astr Soc 91:937–983
Burbank DW, Pinter N (1999) Landscape evolution: the interaction of tectonics and surface processes. Basin res 11:1–6
Bouhadad Y (2001) The Murdjadjo, western Algeria, fault-related fold: implications for seismic hazard. J Seismolog 4(5):541–558
CRAAG (1994) Les séismes en Algérie de 1365 à 1992. Publication du Centre de Recherche en Astronomie, Astrophysique et Géophysique, Département: Etudes et Surveillance Sismique, ESS, C.R.A.A.G, Alger-Bouzaréah
De Mets C, Gordon RC, Argus DF, Stein S (1990) Current plate motion. Geophys J Int 101:425–478
Harbi A, Maouche S, Ayadi A (1999) Neotectonics and associated seismicity in Eastern Tellian Atlas of Algeria. J Seismolog 3:95–104
Jackson J, Norris R, Yougson J (1996) The structural evolution of active fault and fold systems in central Otago, New Zealand: evidence revealed by drainage patterns. J Struct Geol 18:217–234
Keller EA, Gurroba L, Tierney TE (1999) Geomorphic criteria to determine direction of lateral propagation of reverse faulting and folding. Geology 27:515–518
Lavé J, Avouac JP (2001) Fluvial incision and tectonic uplift across the Himalayas of central Nepal. J Geophys Res 106(11):26561–26591
Martinez-Diaz JJ, Masana E, Hernandez-Enrile JL, Santanach P (2003) Effects of repeated paleoearthquakes on the Alhama de Murcia Fault (Betic Cordillera, Spain) on the quaternary evolution of an alluvial fan system. Ann Geopysics 46(5):775–791
Mayer I (1986) Tectonic geomorphology of escarpments and mountains fronts, In: Active tectonics, National academy press, Washington, DC, pp 125–135
Meritts D, Bull WB (1989) Interpreting quaternary uplift rates at the Mendocino triple junction Northern California, from uplifted Marine. Terraces—Geol 17:1020–1024
Molnar P, England P (1990) Late cenozoic uplift of mountain ranges and global mountain changes: chicken or egg? Nature 346:29–34
Pavlis TL, Hamburger MW, Pavlis GL (1997) Erosional processes as a control on the structural evolution of an actively deforming fold and thrust belt: an example from the Pamir-Tien Shan region, central Asia. Tectonics 16:810–822
Scheidegger AE (2004) Morphotectonics. 197 p, Edit. Springer, Berlin
Schumm S (1986) Alluvial river response to active tectonics: in Active tectonics. National academy press, Washington, pp 80–94
Vila J.M., 1980. La chaîne alpine d’Algérie orientale et des confins algéro-tunisiens. Thèse Sci. Univ. Paris, 665 p
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Bouhadad, Y. (2015). Geomorphic Evidence of Active Tectonics: The Case of Djemila Fault (Eastern Algeria). In: Lollino, G., et al. Engineering Geology for Society and Territory - Volume 6. Springer, Cham. https://doi.org/10.1007/978-3-319-09060-3_22
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DOI: https://doi.org/10.1007/978-3-319-09060-3_22
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