Author:
Marco Shmuel,Klinger Yann
Reference124 articles.
1. Abou Romieh M, Westaway R, Daoud M, Bridgland DR (2012) First indications of high slip rates on active reverse faults NW of Damascus, Syria, from observations of deformed Quaternary sediments: implications for the partitioning of crustal deformation in the Middle Eastern region. Tectonophysics 538–540:86–104
2. Agnon A, Migowski C, Marco S (2006) Intraclast breccia layers in laminated sequences: recorders of paleo-earthquakes. In: Enzel Y, Agnon A, Stein M (eds) New Frontiers in Dead Sea paleoenvironmental research. Geological Society of America Special Publication, Boulder, pp 195–214
3. Agnon A, Marco S, Sagy A, Ellenblum R (2010) Discrepancy between GPS (5 yrs) and archaeoseismic (3 kyr) slip rate across the Ateret site (Dead Sea fault): secular variations versus distributed slip. In: Proceedings AGU Fall meeting abstracts, San Francisco, CA, vol 1. American Geophysical Union, p 2206
4. Akyuz HS, Altunel E, Karabacak V, Yalciner CC (2006) Historical earthquake activity of the northern part of the Dead Sea Fault Zone, southern Turkey. Tectonophysics 426:281–293
5. Alchalbi A, Daoud M, Gomez F, McClusky S, Reilinger R, Romeyeh MA, Alsouod A, Yassminh R, Ballani B, Darawcheh R, Sbeinati R, Radwan Y, Masri RA, Bayerly M, Ghazzi RA, Barazangi M (2010) Crustal deformation in northwestern Arabia from GPS measurements in Syria: slow slip rate along the northern Dead Sea Fault. Geophys J Int 180:125–135
Cited by
53 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献