Dynamic fragility of slender and discontinuous rock pillars – an example from the Negev Desert, Israel
Author:
Affiliation:
1. Ben Gurion University of the Negev, Israel
Publisher
The Japanese Geotechnical Society
Link
https://www.jstage.jst.go.jp/article/jgssp/10/60/10_v10.P2-17/_pdf
Reference21 articles.
1. 1) Agnon, A. (2014): Pre-Instrumental Earthquakes Along the Dead Sea Rift. In Z. Garfunkel, Z. Ben-Avraham & E. Kagan (Eds.), Dead Sea Transform Fault System: Reviews (pp. 207-262): Springer.
2. 2) Ambraseys, N. N. (2009): Earthquakes in the Mediterranean and Middle East. A Multidisciplinary Study of Seismicity up to 1900 (1 ed.): Cambridge University Press.
3. 3) Amit, R., Zilberman, E., Porat, N., & Enzel, Y. (1999): Relief Inversion in the Avrona Playa as Evidence of Large-Magnitude Historical Earthquakes, Southern Arava Valley, Dead Sea Rift. Quaternary Research, 52(1), 76-91.
4. 4) Anderson, J. G., Brune, J. N., Biasi, G., Anooshehpoor, A., & Purvance, M. (2011): Workshop Report: Applications of Precarious Rocks and Related Fragile Geological Features to U.S. National Hazard Maps. Seismological Research Letters, 82(3), 431-441.
5. 5) Avni, Y., & Zilberman, E. (2006): Landscape evolution triggered by neotectonics in the Sede Zin region, central Negev, Israel. [Article]. Israel Journal of Earth Sciences, 55(4), 189-208.
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