Tel Re的构造活动与场地形成过程ḥov

IF 0.3 2区 历史学 0 ARCHAEOLOGY
U. Davidovich, E. Zilberman
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引用次数: 0

摘要

Tel Re网站ḥov位于近东最活跃的构造断层带之一——死海裂谷的西部边缘断层上,容易发生构造运动,这对场地形成过程产生了重大影响。作为Tel Re的一部分进行的地质地震和地质考古研究ḥov挖掘项目表明,该遗址位于北部、西部和南部以断层为界的隆起构造块体上。全新世晚期的反复构造活动导致地层和整个土丘向东倾斜,有助于土丘边界的形成,并限制了沉积后侵蚀的程度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Tectonic Activity and Site-Formation Processes at Tel Reḥov
The site of Tel Reḥov is located on one of the most active tectonic fault zones in the Near East—the Western Marginal Fault of the Dead Sea Rift—and was prone to tectonic movements, which had a significant effect on site-formation processes. Geoseismic and geoarchaeological studies conducted as part of the Tel Reḥov excavation project suggest that the site was located on an uplifted tectonic block (horst) bounded by faults on the north, west, and south. Recurrent tectonic activity during the Late Holocene resulted in an eastward-tilting of layers and the entire mound, contributed to the shaping of mound boundaries, and constrained the extent of postdepositional erosion.
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来源期刊
CiteScore
1.10
自引率
0.00%
发文量
41
期刊介绍: Archaeological discoveries continually enrich our understanding of the people, culture, history, and literature of the Middle East. The heritage of its peoples -- from urban civilization to the Bible -- both inspires and fascinates. Near Eastern Archaeology brings to life the ancient world from Mesopotamia to the Mediterranean with vibrant images and authoritative analyses.
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