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GEOPHYSICAL RESEARCH LETTERS,
VOL. 33,
L24314,
doi:10.1029/2006GL027890,
2006
Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization
and crustal rigidity
Uri S. ten Brink
U.S. Geological Survey, Woods Hole, Massachusetts, USA
Abdallah S. Al-Zoubi
Surveying and Geomatics Department, Al-Balqa' Applied University, Salt, Jordan
Claudia H. Flores
U.S. Geological Survey, Woods Hole, Massachusetts, USA
Yair Rotstein
Geophysical Institute of Israel, Lod, Israel
Isam Qabbani
Natural Resources Authority, Amman, Jordan
Steve H. Harder
Department of Geological Sciences, University of Texas at El Paso, El Paso, Texas, USA
G. Randy Keller
Department of Geological Sciences, University of Texas at El Paso, El Paso, Texas, USA
Abstract
New seismic observations from the Dead Sea basin (DSB), a large pull-apart basin along the Dead Sea transform (DST) plate
boundary, show a low velocity zone extending to a depth of 18 km under the basin. The lower crust and Moho are not perturbed.
These observations are incompatible with the current view of mid-crustal strength at low temperatures and with support of
the basin's negative load by a rigid elastic plate. Strain softening in the middle crust is invoked to explain the isostatic
compensation and the rapid subsidence of the basin during the Pleistocene. Whether the deformation is influenced by the presence
of fluids and by a long history of seismic activity on the DST, and what the exact softening mechanism is, remain open questions.
The uplift surrounding the DST also appears to be an upper crustal phenomenon but its relationship to a mid-crustal strength
minimum is less clear. The shear deformation associated with the transform plate boundary motion appears, on the other hand,
to cut throughout the entire crust.
Received 15
August
2006;
accepted 15
November
2006;
published 23
December
2006.
Keywords: Dead Sea;
strain softening;
crustal rheology.
Index Terms: 7203 Seismology: Body waves; 8045 Structural Geology: Role of fluids; 8110 Tectonophysics: Continental tectonics: general (0905); 8118 Tectonophysics: Dynamics and mechanics of faulting (8004); 8168 Tectonophysics: Stresses: general.
Read Full Article (file size: 295016 bytes) Cited by
Citation: ten Brink, U. S., A. S. Al-Zoubi, C. H. Flores, Y. Rotstein, I. Qabbani, S. H. Harder, and G. R. Keller
(2006),
Seismic imaging of deep low-velocity zone beneath the Dead Sea basin and transform fault: Implications for strain localization
and crustal rigidity,
Geophys. Res. Lett.,
33,
L24314,
doi:10.1029/2006GL027890.
Copyright 2006 by the American Geophysical Union.
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