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Unraveling rift margin evolution and escarpment development ages along the Dead Sea fault using cosmogenic burial ages

Published online by Cambridge University Press:  20 January 2017

A. Matmon ,
D. Fink ,
M. Davis ,
S. Niedermann ,
D. Rood  and
A. Frumkin
A. Matmon*
Affiliation:
The Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel
D. Fink
Affiliation:
Australian Nuclear Science and Technology Organization, PMB1, Menai, NSW 2234, Australia
M. Davis
Affiliation:
The Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem 91904, Israel
S. Niedermann
Affiliation:
Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum, Telegrafenberg, D-14473 Potsdam, Germany
D. Rood
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, P.O. Box 808, L-397, Livermore, CA 94550, USA
A. Frumkin
Affiliation:
Department of Geography, The Hebrew University of Jerusalem, Jerusalem 91905, Israel
*
* Corresponding author at: Institute of Earth Sciences Hebrew University of Jerusalem Givat Ram, Jerusalem, Israel 91904. Tel.: + 972 2 6586703; fax: + 972 2 5662581.E-mail address: [email protected] (A. Matmon).
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Abstract

The Dead Sea fault (DSF) is one of the most active plate boundaries in the world. Understanding the Quaternary history and sediments of the DSF requires investigation into the Neogene development of this plate boundary. DSF lateral motion preceded significant extension and rift morphology by ~10 Ma. Sediments of the Sedom Formation, dated here between 5.0 ± 0.5 Ma and 6.2−2.1 +inf Ma, yielded extremely low 10Be concentrations and 26Al is absent. These reflect the antiquity of the sediments, deposited in the Sedom Lagoon, which evolved in a subdued landscape and was connected to the Mediterranean Sea. The base of the overlying Amora Formation, deposited in the terminal Amora Lake which developed under increasing relief that promoted escarpment incision, was dated at 3.3−0.8 +0.9 Ma. Burial ages of fluvial sediments within caves (3.4 ± 0.2 Ma and 3.6 ± 0.4 Ma) represent the timing of initial incision. Initial DSF topography coincides with the earliest Red Sea MORB's and the East Anatolian fault initiation. These suggest a change in the relative Arabian–African plate motion. This change introduced the rifting component to the DSF followed by a significant subsidence, margin uplift, and a reorganization of relief and drainage pattern in the region resulting in the topographic framework observed today.

Keywords

Sedom LagoonAmora LakeCosmogenic burial datingDead Sea fault
Type
Articles
Information
Quaternary Research , Volume 82 , Issue 1 , July 2014 , pp. 281 - 295
Copyright
University of Washington

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