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Dhahal structure : an example of transpression associated with the Dead Sea transform in Wadi Araba, Jordan

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Dhahal Mountains located at the eastern margin of the northern Wadi Araba sinistral fault represent an example of a transpression associated with the Dead Sea transform, which is a sinistral wrench fault. This structure was formed as a result of right bending of the Humrat Fidan active sinistral fault, which is a parallel strand of the Dead Sea transform located east of the main Wadi Araba fault. The fault bend caused uplift and squeezing of the Cretaceous and Tertiary rocks of the transpression. Positive flower structures, folds, fault-bounded wedge-shaped pop-ups and reverse faults are the main structural elements that characterized the Dhahal transpression. Folds are found as sets or as single anticlines and synclines. The major trend of the fold axes is N50°; the principal stress axis (σ1) is perpendicular to this trend (N140°).This trend deviates 26° anticlockwise from that of the Dead Sea stress system (DSS) (as obtained from fault slip data north of the study area), which is responsible for the formation of the Dead Sea transform. Evidence of active uplift in the Dhahal structure is provided by the sharp topography relative to the surrounding areas, and the low mountain front sinuosity index of the western margin of the Dhahal mountains.
Rocznik
Strony
361--370
Opis fizyczny
Bibliogr. 25 poz., fot., rys.
Twórcy
autor
  • Department of Earth and Environmental Sciences, Yarmouk University, Irbid-Jordan
autor
  • Department of Earth and Environmental Sciences, Yarmouk University, Irbid-Jordan
autor
  • Department of Earth and Environmental Sciences, Yarmouk University, Irbid-Jordan
autor
  • Department of Earth and Environmental Sciences, The Hashemite University, Zarqa-Jordan
Bibliografia
  • ABOU KARAKI, N. 1987. Synthèse et carte sismotectonique des pays de la bordure orientale de la Méditerranee: sismicité du système de failes du Jourdan-Mer Morte, Ph. D. Thesis, University of Strasbourg, France.
  • AL-DIABAT, A. 1999. Paleostress and strain analysis of the Cretaceous rocks in the eastern margin of the Dead Sea transform, Jordan, unpub. Ph. D. thesis, University of Baghdad, Baghdad, Iraq.
  • AL-TAJ, M. 2000. Active faulting along the Jordan Valley segment of the Jordan – Dead Sea transform. Ph. D. thesis, University of Jordan, Amman (Unpubl.)
  • AMBRASEYS, N., MELVILLE, C. & ADAMS, R. 1994. The seismicity of Egypt, Arabia and the Red Sea: a historical review. Cambridge University Press; Cambridge.
  • ATALLAH, M. 1986. Application of remote sensing and field techniques to structural problems of the Dead sea Rift in Jordan. Ph. D. Thesis, Technical Univ. Munich Unpublished, 154 pp.
  • — 1992. Tectonic evolution of the northern Wadi Araba, Jordan. Tectonophysics, 204, 17-26.
  • ATALLAH. M., NIEMI, T. & MUSTAFA, H. 2002. Deformation at a strike-slip, stepover zone along the southern margin of the Dead Sea pull-apart basin, Jordan. EGS Stephan Mueller Special Publication Series, 2, 1-21.
  • BEN AVRAHAM, Z. 1985. Structural framework of the Gulf of Elat (Aqaba), Northern Red Sea. Journal of Geophysical Research, 90, 703-726.
  • BOWMAN, D. 1995. Active surface ruptures on the northern Arava fault, the Dead Sea Rift. Israel Journal of Earth Sciences, 44, 51-59.
  • EYAL, Y. 1996. Stress field fluctuations along the Dead Sea rift since the middle Miocene. Tectonics, 15, 157-170.
  • FREUND, R., ZAK, I., GOLDBERG, M., WEISSBROD, T. & DERIN, B. 1970. The shear along the Dead Sea Rift. Philosophical Transactions of the Royal Society of London, A267, 107-130.
  • GALLI, P. 1999. Active tectonics along the Wadi Araba-Jordan Valley transform fault. Journal of Geophysical Research, 104, 2777-2796.
  • GARFUNKEL, Z., ZAK, I. & FREUND, R. 1981. Active faulting in the Dead Sea Rift. Tectonophysics, 80, 1-26.
  • HARLAND, W. 1971. Tectonic transpression in Caledonian Spitsbergen. Geological Magazine, 108, 27-42.
  • KLINGER, Y., AVOUAC, J., ABOU KARAKI, N., DORBATH, L., BOURLES, D. & REYSS, L. 2000. Slip rate on the Dead Sea transform fault in northern Araba valley (Jordan). Geophys. J. Int., 142, 755-768.
  • NIEMI, T., ZHANG, H., ATALLAH, M. & HARRISON, J. 2001. Late Pleistocene and Holocene slip rate of the northern Wadi Araba fault, Dead Sea transform, Jordan. Journal of Seismology, 5, 449-474.
  • POIRIER, J. & TAHER, M. 1980. Historical seismicity in the Near and Middle East, North Africa, and Spain from Arabic documents (VII th-XVIII th century). Bulletin of the Seismological Society of America, 70, 2185-2201.
  • QUENNELL, A. 1958. The structure and evolution of the Dead Sea rift. Quaternary Journal of the Geological Society, 64, 1-24.
  • RABAA, I. 1991. The geology of Al Qurayqira map sheet no. 3015 II. Natural Resources Authority, Amman, Jordan.
  • SANDERSON, D. & MARCHINI, W. 1984. Transpression. Journal of Structural Geology, 6, 449-458.
  • SYLVESTER, A. 1988. Strike slip faults. Geological Society of America Bulletin, 100, 1666-1703.
  • TARAWNEH, B. 1992. The geology of the Fifa Area. Map 3051 I. Amman, Natural Resources Authority of Jordan, scale, 1 : 50 000. 46 pp.
  • WILCOX, R., HARDING, T. & SEELY, D. 1973. Basic wrench tectonics. The American Association of Petroleum Geologist Bulletin, 57, 74-96.
  • ZAK, I. & FREUND, R. 1966. Recent strike slip movement along the Dead Sea Rift. Israel Journal of Earth Sciences, 15, 33-37.
  • ZHANG, H. 1998. Late Pleistocene and Holocene slip rate of the northern Wadi Araba fault, dead Sea transform, Jordan. M. Sc. Thesis, University of Missouri-Kansas city, Unpublished, 128 pp.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-1231-5212
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