A. Bilal / Natural Science 5 (2013) 1019-1024
1024
[8] Molinaro, M., Leturmy, P., Guezou, J.C., Frizon de
Lamotte, D. and Eshraghi, S.A. (2005) The structure and
Kinematic of the southeastern Zagros fold-thrust belt,
Iran: from thin-skinned to thick-skinned tectonics. Tec-
tonics, 24, Article ID: PTC3007.
[9] Agard, P., Monie, P., Gerber, W., Omrani, J., Molinaro,
M., Meyer, B., Labrousse, L., Vrielynk, B., Jolivet, L. and
Yamato, P. (2006) Transient, synobduction exhumation of
Zagros blueschists inferred from P-T, deformation, time,
and kinematic constraints: Implications for newtethyan
wedge dynamics. Journal of Geophysical Research, 111 ,
Article ID: B11401. doi:10.1029/2005JB004103
[10] Cetin, H., Guneyli, H. and Meyer, L. (2003) Paleoseis-
mology of the Palu-Lake hazar segment of the East Ana-
tolian fault zone, Turkey. Tectonophysics, 374, 163-197.
doi:10.1016/j.tecto.2003.08.003
[11] Bosworth, W., Huchon, P. and McClay, K. (2005) The
Red Sea and Gulf of Aden Basin. Journal of Africa Tec-
tonophysics, 209, 115-137.
[12] Barrier, E., Chamot-Rooke, N. and Giordano, G. (2004)
Carte geodynamique de la Méditerranée. Commission de
la Carte Géologique du Monde.
[13] Bilal, A. (2009) Tectono-seismicity and petrological study
of the Syrian rift. Tishreen University Journal for Re-
search Scientific Studies, Basic Scie nces, 31, 127-145.
[14] Bilal, A. and Touret, J.L. (2001) Les enclaves du volcan-
isme récent du rift Syrien. Bulletin de la Societe Geo-
logique de France, 172, 1-14.
[15] Bilal, A. and Sheleh, F. (2004) Un “point chaud” sous le
système du rift Syrien: Données pétrologiques complé-
mentaires sur les enclaves du volcanisme récent. Comptes
Rendus Geoscience, 366, 197-204.
doi:10.1016/j.crte.2003.09.016
[16] Bilal, A. (2009) Seismicity and volcanism in the rifted
zone of western Syria. Comptes Rendus Geoscience, 341,
299-305. doi:10.1016/j.crte.2008.11.005
[17] Bilal, A. and Mahmoud, M. (1997) Soil-structure interac-
tion effect during earthquakes in Syria. International Post -
SMIRT Conference on Seismic Isolation. Taormina, 25-27
August 1997, 837-844.
[18] US Geological Survey (1999) Special report: The hector
mine earthquake 10/16/99.
[19] Khair, K., Karakasis, G.F. and Papadimetriou, E.E. (2000)
Seismic zonation of the Dead Sea transform fault area.
Annali di Geophisica, 43, 61-79.
[20] Meghraui, M., Gomez, F., Sbeinati, R., Woerd, J.V.D.,
Mouty, M., Al-Darkal, A.N., Radwan, Y., Layyons, I., Al
Najjjar, H., Darawcheh, R., Hijazi, F., Al-Ghazzi, R. and
Barazangi, M. (2003) Evidence for 830 years of seismic
quiescence from palaeoseismology, archaeology seismo-
logy, and historical seismicity along the Dead Sea fault in
Syria. Earth and Planetary Science Letters, 210, 35-52.
doi:10.1016/S0012-821X(03)00144-4
[21] Le Béon, M. (2008) Cinématique d’un segment de faille
decrochante à différentes échelles de temps: La faille de
Wadi Araba, segment sud de la faille transformant de
Levant. Thèse Doctorat, Université Paris, VI.
[22] King, G. (2004) Les séismes ne se répètent pas. La Re-
cherche, 380, 14-15.
[23] Maderiaga, R. (2004) Chaque seisme est unique. La Re-
cherche, 275, 14-15.
[24] Taher, M.A. (1979) Documents historiques des tremble-
ments de terre en Syrie depuis l’Islam jusqu’à XII siècle
“hygerique”. Thèse Université, Paris, 300 p.
[25] Al-Tarazi, E. (1999) Regional seismic hazard study for
the eastern Mediterranean (Trans-Jordan, Levant and An-
takia) and Sinai Region. Journal of African Earth Sci-
ences, 3, 743-750. doi:10.1016/S0899-5362(99)00042-1
[26] UNESCO (1983) Assessment and mitigation of earth-
quakes risk in the Arab region. UNESCO, AFESD/IDP.
[27] Stiro, S. (1992) Epicenters of earthquakes from 1961-
1983, USGS. Workshop, Damascus, 32-36.
[28] Sbeinati, M. and Darawcheh, R. (1992) Seismological
bulletin for earthquakes in and around Syria. Report In-
ternational, SAES, Damascus.
[29] Chorowicz, J., Dhont, D., Ammar, O., Rukieh, M. and
Bilal, A. (2005) Tectonics of the Pliocene Homs Basalts
(Syria) and implications for the Dead Sea fault zone ac-
tivity. Journal of the geological Society, London, 162,
259-271.
[30] Rojay, B., Heimann, A. and Toprak, V. (2001) Neotec-
tonic and volcanic characteristics of the Karasu fault zone
(Anatolia, Turkey): The transition between the Dead Sea
Transform and the East Anatolian fault zone. Geody-
namica Acta, 14, 197-212.
doi:10.1016/S0985-3111(00)01053-6
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