scholarly journals GPS measurements of near-field deformation along the southern Dead Sea Fault System

2011 ◽  
Vol 12 (12) ◽  
pp. n/a-n/a ◽  
Author(s):  
Eid al Tarazi ◽  
Jafar Abu Rajab ◽  
Francisco Gomez ◽  
William Cochran ◽  
Rani Jaafar ◽  
...  
2021 ◽  
Vol 60 (1) ◽  
pp. 31-50
Author(s):  
Ryad Darawcheh ◽  
Riad Al Ghazzi ◽  
Mohamad Khir Abdul-wahed

In this research, a data set of horizontal GPS coseismic displacement in the near-field has been assembled around the world in order to investigate a potential relationship between the displacement and the earthquake parameters. Regression analyses have been applied to the data of 120 interplate earthquakes having the magnitude (Mw 4.8-9.2). An empirical relationship for prediction near-field horizontal GPS coseismic displacement as a function of moment magnitude and the distance between hypocenter and near field GPS station has been established using the multi regression analysis. The obtained relationship allows assessing the coseismic displacements associated with some large historical earthquakes occurred along the Dead Sea fault system. Such a fair relationship could be useful for assessing the coseismic displacement at any point around the active faults.


2020 ◽  
Vol 221 (3) ◽  
pp. 1913-1940
Author(s):  
Francisco Gomez ◽  
William J Cochran ◽  
Rayan Yassminh ◽  
Rani Jaafar ◽  
Robert Reilinger ◽  
...  

SUMMARY A comprehensive GPS velocity field along the Dead Sea Fault System (DSFS) provides new constraints on along-strike variations of near-transform crustal deformation along this plate boundary, and internal deformation of the Sinai and Arabian plates. In general, geodetically derived slip rates decrease northwards along the transform (5.0 ± 0.2 to 2.2 ± 0.5 mm yr−1) and are consistent with geological slip rates averaged over longer time periods. Localized reductions in slip rate occur where the Sinai Plate is in ∼N–S extension. Extension is confined to the Sinai side of the fault and is associated with prominent changes in transform geometry, and with NW–SE striking, left-lateral splay faults, including the Carmel Fault in Israel and the Roum Fault in Lebanon. The asymmetry of the extensional velocity gradients about the transform reflects active fragmentation of the Sinai Plate along the continental margin. Additionally, elastic block modelling of GPS velocities requires an additional structure off-shore the northern DSF segment, which may correspond with a fault located along the continental margin, suggested by prior geophysical studies.


1998 ◽  
Author(s):  
Uri S. ten Brink ◽  
M. Rybakov ◽  
A. Al-Zoubi ◽  
M. Hassouneh ◽  
A. Batayneh ◽  
...  

2003 ◽  
Vol 153 (3) ◽  
pp. 658-674 ◽  
Author(s):  
Francisco Gomez ◽  
Mustapha Meghraoui ◽  
Abdul Nasser Darkal ◽  
Fouad Hijazi ◽  
Michel Mouty ◽  
...  

2017 ◽  
Vol 18 (3) ◽  
pp. 844-857 ◽  
Author(s):  
P. Censi ◽  
M. Raso ◽  
Y. Yechieli ◽  
H. Ginat ◽  
F. Saiano ◽  
...  

2001 ◽  
Vol 158 (4) ◽  
pp. 665-674 ◽  
Author(s):  
GRAHAM BREW ◽  
JACEK LUPA ◽  
MUAWIA BARAZANGI ◽  
TARIF SAWAF ◽  
ANWAR AL-IMAM ◽  
...  

Tectonics ◽  
1990 ◽  
Vol 9 (6) ◽  
pp. 1369-1386 ◽  
Author(s):  
Thomas A. Chaimov ◽  
Muawia Barazangi ◽  
Damen Al-Saad ◽  
Tarif Sawaf ◽  
Ali Gebran

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