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Dead Sea Transform? Anyone please explain if you know?

What I know is ,it's a fault line. Am I right?

3 Answers

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  • Anonymous
    1 decade ago
    Favorite Answer

    To address one of the central questions of plate tectonics - How do large transform

    systems work and what are their typical features? - geophysical investigations across

    the Dead Sea Transform (DST), the boundary between the African and Arabian plates

    in the Middle East, were conducted for the first time and combined with 2.5 and 3D

    thermo-mechanical modelling. One major component of these investigations are seismic

    and seismological surveys across the Dead Sea Transform. Main results of this

    study indicate that the DST cuts through the entire crust, that strong lower crustal reflectors

    are imaged only on one side of the DST, that the seismic velocity sections

    show a steady increase in the depth of the crust Moho from 26 km at the Mediterranean

    to 39 km under the Jordan highlands, with only a small but visible, asymmetric

    topography of the Moho under the DST. The SKS splitting study demonstrate that a

    distinct narrow (30 km wide) vertical zone in the mantle exists under the DST with the

    seismic anisotropy consistent with the shear deformation between decoupled, Arabian

    and the African plates.

    These observations are replicated and integrated by the extended 2D (2.5D) thermomechanical

    numerical model focused on lithospheric-scale deformation at the DST.

    This model demonstrates that all these observations can be linked to the left-lateral

    movement of 105 km of the two plates in the last 17 Ma, accompanied by strong deformation

    within a 20-30 km wide zone cutting through the entire crust and mantle

    lithosphere. The modelling results also clearly indicate that the DST in the Arava Valley

    is almost pure strike-slip boundary with less than 4 km of transform-perpendicular

    extension (rifting deformation component). The preliminary results of the 3D thermomechanical

    model, which incorporates the Dead Sea basin, shows that even this small

    rifting component may be unnecessary to explain observed crustal structure.

    Source(s): http://209.85.207.104/search?q=cache:nKw00b0WaAMJ:... www.cosis.net/abstracts/EGU05/09814/EGU05-J-09814.pdf
  • 1 decade ago

    It is called the Dead Sea Rift. The Great Rift Valley faultline runs through part of the Dead Sea region and the Mount of Olives. A major earthquake has struck the Dead Sea Basin roughly every 100 years, and seismologists believe that the next big earthquake is overdue. They have warned that Israel is not prepared to deal with the aftermath of such an event, which could leave up to 16,000 dead and thousands more homeless.

  • Anonymous
    1 decade ago

    no more coffee you need a nap...

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