The reconstruction of the seismic history of an archaeological site is generally based on historical sources and/or archaeoseismological data. However, these data alone give, in most of the cases, only qualitative information and cannot be used to unequivocally recognize the kinematics of past earthquakes and causative fault. A multidisciplinary approach merging archaeological information and geological data is useful to better constrain the age of past earthquakes, identify the fault movement(s), and clarify the seismotectonic picture of a region. The Hisham palace (724–743 A.D. to about 1400 A.D.; Baramki, 1936, 1938; Whitcomb, 1988), which is the main...
The Kinematics of the 1033 A.D. Earthquake Revealed by the Damage at Hisham Palace (Jordan Valley, Dead Sea Transform Zone)
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L. Alfonsi, F. R. Cinti, G. Ventura; The Kinematics of the 1033 A.D. Earthquake Revealed by the Damage at Hisham Palace (Jordan Valley, Dead Sea Transform Zone). Seismological Research Letters ; 84 (6): 997–1003. doi: https://doi.org/10.1785/0220130060
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