Advanced Search

Indexed by SCI、CA、РЖ、PA、CSA、ZR、etc .

Volume 26 Issue 5
Oct 2015
Turn off MathJax
Article Contents
Mohammed Fnais, Abdullah Al-Amri, Kamal Abdelrahman, Enayat Abdelmonem, Sherif El-Hady. Seismicity and Seismotectonics of Jeddah-Makkah Region, West-Central Saudi Arabia. Journal of Earth Science, 2015, 26(5): 746-754. doi: 10.1007/s12583-015-0587-y
Citation: Mohammed Fnais, Abdullah Al-Amri, Kamal Abdelrahman, Enayat Abdelmonem, Sherif El-Hady. Seismicity and Seismotectonics of Jeddah-Makkah Region, West-Central Saudi Arabia. Journal of Earth Science, 2015, 26(5): 746-754. doi: 10.1007/s12583-015-0587-y

Seismicity and Seismotectonics of Jeddah-Makkah Region, West-Central Saudi Arabia

doi: 10.1007/s12583-015-0587-y
More Information
  • Corresponding author: Kamal Abdelrahman, khassanein@ksu.edu.sa
  • Received Date: 07 Oct 2012
  • Accepted Date: 27 Mar 2013
  • Publish Date: 01 Oct 2015
  • Jeddah-Makkah regionis have been suffering from earthquake crisis where some moderate to destructive earthquakes have been recorded. These earthquake activities are oriented along major faults or clustered in certain spots. Moreover, these earthquake events have annual recurrence periods, so the identification of these seismogenic source zones is of utmost importance for mapping the most hazardous localities which should be avoided in the future urban planning. Historical and instrumental earthquakes have been collected from national and international data centers and unified in catalogue. The existence of microearthquakes inland suggests that there is a significant level of tectonic activity at away from the axial trough of the Red Sea. Then, seismogenic source zones have been defined depending on the major tectonic trends; distribution of earthquake epicenters, seismicity rate (a & b-values) and fault plane solution of major earthquakes. It is concluded that Jeddah-Makkah region is affected by the outlined five seismogenic source zones; three of these zones aligned of the main Red Sea axial trough (southwestern Jeddah, western Jeddah, and northwestern Jeddah zones), while the other two zones are located in the land area of the region (Thewal-Rabegh and Jeddah-Makkah zones). These inland zones correlated well with the main trends of major tectonics which refleet the reactivation of tectonic movements along these fault trends. The Red Sea zones are in agreement with the main path of the axial trough. The range of b-value in these identified zones is 0.65 to 1.03 through these identified zones. The area characterized by higher b-values could be indicative of a relative low stress regime which was a result of resulting from the stress release by the earthquakes. Whereas, the areas of lower b-values can be considered as an evidence of a relatively higher stress regime associated with a dominantly extensional stresses. Based on aforementioned, the region is suffering from different stress level accumulations which, in turn, cause earthquakes with different magnitudes. Accordingly, deployment of local seismograph network through Jeddah-Makkah region is highly recommended. These results will support, to a great extent, seismic hazard assessment and risk mitigation of the region.

     

  • loading
  • Al-Arifi, N. S., 2002. Focal Mechanism of the 1988, 1993, 1994, 1995, and 1996 Southern Red Sea Sequences Activity, Bulletin of the Faculty of Science, 29(2): 33–54
    Al-Furaih, A. A., Al-Aswad, A. A., Kebeasy, R. M., 1994. New Aspects on Estimated Risk around the Makkah Region. 2nd Ann. Meeting of Saudi. Soc. of Earth Sci. , 19: 25–27
    Alwash, M., Zakir, F, . 1992. Tectonic Analysis of the Jeddah Taif Area on the Basis of LANDSAT Satellite Data. Journal of African Earth Sciences, 15(2): 293–300
    Al-Garni, M., 2009. Geophysical Investigations for Groundwater in a Complex Subsurface Terrain, Wadi Fatima, KSA: A Case History. Jordan Journal of Civil Engineering, 3(2): 118–136 http://www.researchgate.net/publication/320434111_Geophysical_investigations_for_groundwater_in_a_complex_subsurface_terrain_Wadi_Fatima_KSA_A_case_history
    Al-Garni, M., El-Behiry, M., Gobash, M., 2012. Geophysical Survey for Geological Hazards Assessment of Wadi Thuwal Area, KSA: A Case History. Arab J. Geosci. 5(1): 133–146 Doi: 10.1007/s12517-010-0147-9.
    Al-Saud, M., 2008. Seismic Characteristics and Kinematic Models of Makkah and Central Red Sea Regions. Arab. J. Geosciences, 1: 49–61 doi: 10.1007/s12517-008-0004-2
    AI-Shanti, A. M. S., 1966. Oolitic Iron Ore Deposits in Wadi Fatima between Jeddah and Makkah, Saudi Arabia. DGMR Bulletin, 2: 1–29 http://ci.nii.ac.jp/ncid/BA52210892
    Azzedine, B., Ritz, J., Philip, H., 1998. Drainage Diversions as Evidence of Propagating Faults: Example of the El Asnam and Thenia Faults, Algeria. Terra Nova, 10: 236–244 doi: 10.1046/j.1365-3121.1998.00197.x
    Coleman, R. G., 1984. The TihamatAsir Igneous Complex: A Passive Margin Ophiolite, Proceedings of International Geological Congress, 27th, Moscow. 9: 221–239
    Davies, G.F., 1984. Geophysical and Isotopic Constraints on Mantle Convection—An Interim Synthesis. Journal of Geophysical Research, 89 (7): 617–640 http://adsabs.harvard.edu/abs/1984JGR....89.6017D
    El-Isa, Z. H., Al-Shanti, A., 1989. Seismicity and Tectonics of the Red Sea and Western Arabia. Geophysical Journal, 97: 449–457 doi: 10.1111/j.1365-246X.1989.tb00515.x
    Farrell, J., Stephan Husen, S., Smith, R., 2009. Earthquake Swarm and b-Value Characterization of the Yellowstone Volcano-Tectonic System. Journal of Volcanology and Geothermal Research, 188: 260–276 doi: 10.1016/j.jvolgeores.2009.08.008
    Fleck, R. J., Greenwood, W. R., Hadley, D. G., et al., 1980. Rubidium-Strontium Geochronology and the Plate-Tectonic Evolution of the Southern Part of the Arabian, Shield. U.S. Geol. Survey Prof. paper. 1131 http://www.sciencedirect.com/science/article/pii/B9780080244792500055
    Gardner, J. K., Knopoff, L., 1974. Is the Sequence of Earthquake in Southern California, with Aftershocks Removed, Poissonian? Bull. Seism. Soc. Am. , 64: 1363–1367
    Greenwood, W. R., Hdley, D. G., Anderson, R. E., et al., 1976. Late Proterozoiccratonization in S.W. Saudi Arabia. Philosophical Transaction of the Royal Society of London, 280: 3–38 http://rsta.royalsocietypublishing.org/content/280/1298/517.abstract
    Hansen, S. A., Rodgers, S. S., Al-Amri, A., 2007. Imaging Ruptured Lithosphere beneath the Red Sea and Arabian Peninsula. Earth and Planetary Science Letter, 259: 256–265. doi: 10.1016/j.epsl.2007.04.035
    Lopoukhine, M., Stieltjes, L., 1974. Geothermal Reconnaissance in the Kingdom of Saudi Arabia. BRGM 76-JED-18.
    Merghelani, H. M., Gallanthine, S. K., 1981. Microearthquakes in the Tihamat-Asir Region of Saudi Arabia. Bull. Seism. Soc. Am. , 70(6): 2291–2293 http://www.researchgate.net/publication/284040991_Microearthquakes_in_the_Tihamat-Asir_region_of_Saudi_Arabia
    Moore, T. A., Al-Rehaili, M. H., 1989. Geologic Map of the Makkah Quadrangle, Sheet 21D, Kingdom of Saudi Arabia, Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources Publication, Jeddah, K.S.A.
    Mogi, K., 1962. Magnitude-Frequency Relationship for Elastic Shocks Accompanying Fractures of Various Materials and Some Related Problems in Earthquakes. Bull. Earthquake Res. Inst. Univ. Tokyo, 40: 831–883 http://www.researchgate.net/publication/29773832_Magnitude-Frequency_Relation_for_Elastic_Shocks_Accompanying_Fractures_of_Various_Materials_and_Some_Related_problems_in_Earthquakes_2nd_Paper
    Nebert, K., Al-Shaibi, A. A., Awlia, M., et al., 1974. Geology of the Area North Wadi Fatima, Kingdom of Saudi Arabia. Journal of King Abdulaziz Univ., Earth Sci. , 1. 294 http://www.getcited.org/pub/101640592
    Qari, M., 2009. Geomorphology of Jeddah Governate, with Emphasis on Drainage Systems. Journal of King Abdulaziz Univ., Earth Sci. , 20(1): 93–116
    Schmidt, D. L., Hadley, D. G., Brown, G. F., 1982. Middle Tertiary Continental Drift and Evolution of the Red Sea in Southwestern Saudi Arabia, Saudi Arabian. Deputy Ministry of Mineral Resources (DGMR), Open File Report USGSOF-03-6-56P.
    Scholz, C. H., 1968. The Frequency-Magnitude Relation of Microfracturing in Rock and its Relation to Earthquakes. Bull. Seismol. Soc. Am., 58: 399–415 doi: 10.1785/BSSA0580010399
    Scordilis, E. M., 2006. Empirical Global Relations Converting Ms and Mb to Moment Magnitude. Journal of Seismology, 19: 225–236 http://gji.oxfordjournals.org/external-ref?access_num=10.1007/s10950-006-9012-4&link_type=DOI
    Skiba, W. J., Tayeb, J., AI-Khatieb, S. O., et al., 1977. Geology of the Jeddah-Makkah Area (21/39), Kingdom of Saudi Arabia. Saudi Arabian Directorate General of Mineral Resources (Unpublished Bulletin)
    Stern, R. J., 1985. The Najd Fault System, Saudi Arabia and Egypt. A Late Precambrian Rift-Related Transform System. Tectonics, 4: 497–511 doi: 10.1029/TC004i005p00497
    Swolfs, H. S., 1994. Listing of Earthquakes in the Arabian Tectonic Plate. USGS-DFR-94-3.29
    Wyss, M., 1973. Towards a Physical Understanding of the Earthquake Frequency Distribution. Geophys. J.R. Astr. Soc. , 31: 341–359 doi: 10.1111/j.1365-246X.1973.tb06506.x
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(12)  / Tables(3)

    Article Metrics

    Article views(715) PDF downloads(109) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return