| Preliminary Analysis of Tectonic Deformation Phenomena in Some Archaeological Sites in Shandong Province |
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| 作者姓名： | Zheng Haigang Yang Yuanyuan Yao Daquan Zhao Peng Gong Xicheng Shen Xiaoqi |
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| 作者单位： | Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Earthquake Administration of Anhui Province, Hefei 230031, China,Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Cultural Relic Institute of Archaeology of Anhui Province, Hefei 230001, China,Earthquake Administration of Anhui Province, Hefei 230031, China |
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| 基金项目： | This paper was jointly supported by the Anhui Public Welfare Geological Project (No. 2015-g-25) and the Special Research Project of CEA (No. TYZ20160101). |
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| 摘 要： | Earthquake archaeological research was conducted in recent years at four archaeological excavation sites in Shandong, focusing on the identification and analysis of the tectonic deformation phenomena. The non-tectonic deformation phenomena were distinguished at the site of the Shang Dynasty ruins at Daxinzhuang in the Jinan suburbs. In Longshan, sand vein-filled cracks were recognized in the cultural layers of the Chengziya site, Zhangqiu City. Sand veins on the trench wall and sand tubes at the trench bottom were found densely distributed at the Shang and Zhou Dynasty cultural layers, at Qinhuangtai site, Binzhou City. The tectonic and non-tectonic origin cracks were identified on the city wall of the Site of Capital of State Qi, Linzi City. In Rizhao city, parallel distributed sand vein fracture groups were found in the cultural layer of Longshan-Warring States-Han Dynasty at Yaowangcheng site. Typical conjugate shear fractures were identified on the city wall of the ancient city of the State of Xue, Tengzhou City. The above natural deformation phenomena are concentrated in the culture layers of the Spring and Autumn-Warring States-Han Dynasties and before, and characterized by seismic sand-soil liquefaction traces, which indicate that these regions might have been in the seismic active episodes in the corresponding periods. The above inference has been confirmed by microscopic data analysis.
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| 关 键 词： | Shandong Archaeoseismology Tectonic Deformation The Warring States Period-Han Dynasty |
| 收稿时间： | 2015/1/6 0:00:00 |
| 修稿时间： | 2015/9/30 0:00:00 |
Preliminary Analysis of Tectonic Deformation Phenomena in Some Archaeological Sites in Shandong Province |
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| Zheng Haigang,Yang Yuanyuan,Yao Daquan,Zhao Peng,Gong Xicheng,Shen Xiaoqi.Preliminary Analysis of Tectonic Deformation Phenomena in Some Archaeological Sites in Shandong Province[J].Earthquake Research in China,2017,31(4):513-526. |
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| Authors: | Zheng Haigang Yang Yuanyuan Yao Daquan Zhao Peng Gong Xicheng and Shen Xiaoqi |
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| Institution: | Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Earthquake Administration of Anhui Province, Hefei 230031, China,Earthquake Administration of Anhui Province, Hefei 230031, China;Mengcheng National Geophysical Observate, Mengcheng 233500, Anhui, China,Cultural Relic Institute of Archaeology of Anhui Province, Hefei 230001, China and Earthquake Administration of Anhui Province, Hefei 230031, China |
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| Abstract: | Earthquake archaeological research was conducted in recent years at four archaeological excavation sites in Shandong, focusing on the identification and analysis of the tectonic deformation phenomena. The non-tectonic deformation phenomena were distinguished at the site of the Shang Dynasty ruins at Daxinzhuang in the Jinan suburbs. In Longshan, sand vein-filled cracks were recognized in the cultural layers of the Chengziya site, Zhangqiu City. Sand veins on the trench wall and sand tubes at the trench bottom were found densely distributed at the Shang and Zhou Dynasty cultural layers, at Qinhuangtai site, Binzhou City. The tectonic and non-tectonic origin cracks were identified on the city wall of the Site of Capital of State Qi, Linzi City. In Rizhao city, parallel distributed sand vein fracture groups were found in the cultural layer of Longshan-Warring States-Han Dynasty at Yaowangcheng site. Typical conjugate shear fractures were identified on the city wall of the ancient city of the State of Xue, Tengzhou City. The above natural deformation phenomena are concentrated in the culture layers of the Spring and Autumn-Warring States-Han Dynasties and before, and characterized by seismic sand-soil liquefaction traces, which indicate that these regions might have been in the seismic active episodes in the corresponding periods. The above inference has been confirmed by microscopic data analysis. |
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| Keywords: | Shandong Archaeoseismology Tectonic Deformation The Warring States Period-Han Dynasty |
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