Abstract
The Mahelma fault, located upon the Sahel anticline at the tip of the major Sahel fault, is often suspected to be a secondary structure. Yet, to date, the Mahelma fault has displayed no definitive evidences for faulting activity and no unambiguous typology. This paper reviews new data, especially geological and subsurface data, acquired through the Algiers west microzoning project. The data indicate that (1) the Mahelma fault is an antithetic high-angle reverse fault, (2) the interpreted dip is around 80° toward the SSE and thus implies a North-verging fault, and (3) the fault zone has been observed in several fault sites and allowed direct observation of fault displacements and fault throws. (4) Displacements directly related to the Mahelma fault affect clearly young sediments including consolidated Quaternary sands. We suggest that the Mahelma fault forms an active backthrust originating from pre-existing normal fault with a possible linkage and interaction with the major Sahel forethrust. We conclude from the foregoing that the Mahelma fault most likely ruptures in concert with earthquakes on the Sahel main fault. The results also point the activity of the Sahel fault-related fold and hence complicate earthquake hazard analyses.
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References
Aifa T, Feinberg H, Derder MEM, Merabet N (1992) Rotations paleomagnetiques récentes dans le bassin du Cheliff (Algérie). CR Acad Sci Paris 314:915–922
Aymé A (1952) Le Quaternaire littoral des environs d’Alger. In: Actes du Congrès Panafricain de Préhistoire. IIe session, Alger, pp 242–246
Aymé A (1954) Service de la Carte Géologique de l'Algérie, Étude des Terrains Néogènes de la Cluse du Mazafran:(Sahel d'Alger)
Betrouni M (1983) Le pléistocène supérieur du littoral ouest algérois.Doctoral dissertation, Universitéd'Aix-Marseille II, Fac. Sc. Luminy, pp 202, 52
Boudiaf A (1996) Etude sismotectonique de la région d'Alger et de la Kabylie (Algérie): utilisation des modèles numériques de terrains (MNT) et de la télédétection pour la reconnaissance des structures tectoniques actives: contribution à l'évaluation de l'aléa sismique.Doctoral dissertation, Université de Montpellier 2
Chester JS, Chester FM (1990) Fault-propagation folds above thrusts with constant dip. Journal of Structural Geology 12(7):903–910
CGS Internal Report (2009) Microzonage sismique de la ville nouvelle de Sidi Abdellah
Dahlin T, Zhou B (2004) A numerical comparison of 2D resistivity imaging with 10 electrode arrays. Geophys Prospect 52(5):379–398
Dalloni M (1940) Notes sur la classification du Pliocène supérieur et du Quaternaire de l'Algérie. Bull Soc Géog D’Oran:8–43
Davis K, Burbank DW, Fisher D, Wallace S, Nobes D (2005) Thrust-fault growth and segment linkage in the active Ostler fault zone, New Zealand. J Struct Geol 27(8):1528–1546
Delouis B, Vallée M, Meghraoui M, Calais E, Maouche S, Lammali K et al (2004) Slip distribution of the 2003 Boumerdes–Zemmouri earthquake, Algeria, from teleseismic, GPS, and coastal uplift data. Geophys Res Lett 31:L18607. https://doi.org/10.1029/2004GL020687
Derder MEM, Henry B, Maouche S, Bayou B, Amenna M, Besse J, Bessedik M, Belhai D, Ayache M (2013) Transpressive tectonics along a major E-W crustal structure on the Algerian continental margin: blocks rotations revealed by a paleomagnetic analysis. Tectonophysics 593:183–192
Erslev EA, Mayborn KR (1997) Multiple geometries and modes of fault-propagation folding in the Canadian thrust belt. J Struct Geol 19(3–4):321–335
Fossen H (2010) Structural geology. Cambridge University Press, pp 463
Giambiagi L, Ghiglione M, Cristallini E, Bottesi G (2009) Kinematic models of basement/cover interaction: insights from the Malargüe fold and thrust belt, Mendoza, Argentina. J Struct Geol 31(12):1443–1457
Glangeaud L (1952) Histoire géologique de la province d'Alger.XIX international geological congress Algiers, regional Monographs first series, Algeria
Heddar A, Authemayou C, Djellit H, Yelles AK, Déverchère J, GharbiS LBVV (2013) Preliminary results of a paleoseismological analysis along the Sahel fault (Algeria): new evidence for historical seismic events. Quat Int 302:210–223
INCT (1999) Aerial photographs compaign of the Koléa-Mahélma Region. 1/20 000 scale
Kelsey HM, Sherrod BL, Nelson AR, Brocher TM (2008) Earthquakes generated from bedding plane-parallel reverse faults above an active wedge thrust, Seattle fault zone. Geol Soc Am Bull 120(11–12):1581–1597
Lee JC, Chu HT, Angelier J, Chan YC, Hu JC, Lu CY, Rau RJ (2002) Geometry and structure of northern surface ruptures of the 1999 Mw= 7.6 Chi-Chi Taiwan earthquake: influence from inherited fold belt structures. J Struct Geol 24(1):173–192
Loke MH (2012) Tutorial: 2-D and 3-D electrical imaging surveys. GeotomoSoftware, Malaysia
Loke MH, Barker RD (1996) Rapid least-squares inversion of apparent resistivity pseudosections by a quasi-Newton method 1. Geophys Prospect 44(1):131–152
Loke MH, Dahlin T (2002) A comparison of the Gauss–Newton and quasi-Newton methods in resistivity imaging inversion. J Appl Geophys 49(3):149–162
Maouche S (2010) Tectonique active et géodynamique de long de l'Atlas Tellien étude des soulèvements côtiers. Doctoral dissertation, Université des sciences et de la technologie Houari Boumediene
Maouche S, Harbi A (2018) The active faults of the Mitidja basin (north Central Algeria): what does the seismic history of the region tell us?. A review. Euro-Mediterr J Environ Integr. https://doi.org/10.1007/s41207-018-0061-1
Maouche S, Meghraoui M, Morhange C, Belabbes S, Bouhadad Y, Haddoum H (2011) Active coastal thrusting and folding, and uplift rate of the Sahel anticline and Zemmouri earthquake area (Tell Atlas, Algeria). Tectonophysics 509(1–2):69–80
Mauffret A, El Robrini M, Genesseaux M (1987) Indice de la compression récente en mer Méditerranée : un bassin losangique sur la marge algérienne. Bull de la Soc Géol de France 8(6):1195–1206. https://doi.org/10.2113/gssgfbull.III.6.1195
Mccalpin JP (2009) Paleoseismology. In: International Geophysics Series, 2nd edn. Academic Press, London, p 613
McClay KR (1992) Glossary of thrust tectonics terms. Thrust Tectonics:419–433
McClay KR and Buchanan PG (1992) Thrust faults in inverted extensional basins. Thrust tectonics, 93–104
McLaren MK, Hardebeck JL, Van DEN, Unruh JR, Bawden GW, Blair JL (2008) Complex faulting associated with the 22 December 2003 M w 6.5 San Simeon, California, earthquake, aftershocks, and postseismic surface deformation. Bull Seismol Soc Am 98(4):1659–1680
Meghraoui M (1988) Géologie des zones sismiques du Nord de l'Algérie:Paléosismologie, tectonique active et synthèse sismotectonique. Doctoral dissertation, UnivrsitéParis 11
Meghraoui M (1991) Blind reverse faulting system associated with the Mont Chenoua-Tipaza earthquake of 29 October 1989 (north-Central Algeria). Terra Nova 3(1):84–92
Meghraoui M, Pondrelli S (2012) Active faulting and transpression tectonics along the plate boundary in North Africa. Ann Geophys 55(5):955–967. https://doi.org/10.4401/ag-4970
Mitra S (2002) Fold-accommodation faults. AAPG Bull 86(4):671–693
Morel JL, Meghraoui M (1996) Goringe-Alboran-tell tectonic zone: a transpression system along the Africa-Eurasia plate boundary. Geology 24(8):755–758
Moulouel H, Bensalem R, Machane D, Bendaoud A, Gharbi S, Oubaiche EH, Ousalem H, Skendri W (2017) High resistant sand injected marl and low resistant damaged marl to locate and characterize the Thenia fault zone in Boumerdes City (North-Central Algeria). Pure Appl Geophys 174:103–115. https://doi.org/10.1007/s00024-016-1400-2
Neely TG, Erslev EA (2009) The interplay of fold mechanisms and basement weaknesses at the transition between Laramide basement-involved arches, north-central Wyoming, USA. J Struct Geol 31(9):1012–1027
Nelson AR, Johnson SY, Kelsey HM, Wells RE, Sherrod BL, Pezzopane SK, Bucknam RC (2003) Late Holocene earthquakes on the toe Jam Hill fault, Seattle fault zone, Bainbridge Island, Washington. Geol Soc Am Bull 115(11):1388–1403
Niño F, Philip H, Chéry J (1998) The role of bed-parallel slip in the formation of blind thrust faults. J Struct Geol 20(5):503–516
Nocquet JM, Calais E (2004) Geodetic measurements of crustal deformation in the Western Mediterranean and Europe. Pure Appl Geophys 161(3):661–681
Philip H, Meghraoui M (1983) Structural analysis and interpretation of the surface deformations of the El Asnam earthquake of October 10, 1980. Tectonics 2(1):17–49
Saoudi NE (1989) Pliocène et Pléistocène inférieur et moyen du Sahel occidental d'Alger. Entreprise nationale du livre
Schultz RA (2000) Localization of bedding plane slip and backthrust faults above blind thrust faults: keys to wrinkle ridge structure. J Geophys Res: Planets 105(E5):12035–12052
Thomas G (1985) Géodynamique d'un bassin intra montagneux : le bassin du bas Chéliff occidental (Algérie) durant le Mio-Plio-Quaternaire. PhD thesis, Pau Univ, France
Wells DL, Coppersmith KJ (1994) New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement. Bull Seismol Soc Am 84(4):974–1002
Yielding G, Ouyed M, King GCP, Hatzfeld D (1989) Active tectonics of the Algerian Atlas Mountains: evidence from aftershocks of the 1980 El Asnam earthquake. Geophys J Int 99(3):761–788
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The Authors thank the chief editor and anonymous reviewer for their constructive comments that improved the manuscript.
Funding
This research has been funded by the “Institut National de Recherche Appliquée en Génie-Parasismique (CGS)” through the Algiers West Microzoning Project, including “The Surface Ruptures of Mahelma Fault” conducted by Moulouel Hakim.
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Moulouel, H., Bouchelouh, A., Bensalem, R. et al. The Mahelma fault: a secondary structure of the Sahel anticline?. Arab J Geosci 13, 715 (2020). https://doi.org/10.1007/s12517-020-05694-z
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DOI: https://doi.org/10.1007/s12517-020-05694-z