Timing of earthquake ruptures at the Al Harif Roman aqueduct (Dead Sea fault, Syria) from archaeoseismology and paleoseismology
Timing of earthquake ruptures at the Al Harif Roman aqueduct (Dead Sea fault, Syria) from archaeoseismology and paleoseismology
复制标题
根据考古地震学和古地震学确定的 Al Harif 罗马渡槽（叙利亚死海断层）地震破裂的时间
DOI：
10.1130/2010.2471(20
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发表时间：
2010
影响因子：
1.9
通讯作者：
R. Al
中科院分区：
文献类型：
--
作者：
M. R. Sbeinati;M. Meghraoui;Ghada Suleyman;F. Gomez;P. Grootes;M. Nadeau;Haithem Al Najjar;R. Al
我们研究了位于死海断层北向约90公里长的Missyaf段的Al Harif罗马渡槽，使用了四次考古发掘，三条古地震壕沟，以及六个凝灰岩岩芯的分析。渡槽围墙的破坏表现为自渡槽建造以来连续的左旋断层错动，达13.6±0.2m，断代时间早于公元前65年。槽沟沉积单元、渡槽围墙的建筑胶结物和凝灰岩芯的放射性碳测年制约了渡槽的晚期历史。建筑石材的类型，
We studied the faulted Al Harif Roman aqueduct, located on the north–trending, ~90-km-long Missyaf segment of the Dead Sea fault, using four archaeological excavations, three paleoseismic trenches, and the analysis of six tufa cores. Damage to the aqueduct wall exhibits successive left-lateral fault offsets that amount to 13.6 ± 0.2 m since the aqueduct construction, which is dated younger than 65 B.C. Radiocarbon dating of sedimentary units in trenches, building cement of the aqueduct wall, and tufa cores constrain the late Holocene aqueduct history. The building stone types,