德国社会学家韦伯(Max Weber,1864-1920)与奥地利法学家凯尔森(Hans Kelsen,1881-1973)对"法律社会学"(Rechtssoziologie,sociology of law)的定位存在异同。他们一个从社会学家的立场,一个从法学家的立场,探讨了"法律...德国社会学家韦伯(Max Weber,1864-1920)与奥地利法学家凯尔森(Hans Kelsen,1881-1973)对"法律社会学"(Rechtssoziologie,sociology of law)的定位存在异同。他们一个从社会学家的立场,一个从法学家的立场,探讨了"法律社会学"在19世纪末叶跟着社会学(Soziologie)一起诞生的时候,究竟应该如何对这新兴的学问加以定位的问题。他们两位都是法学家出身,同样受到当时哲学思潮新康德主义(Neukantianismus)的影响,主张划分"实然"(Sein)与"应然"(Sollen),也同样对促进德语世界法律社会学的诞生有积极贡献的"自由法学派"(Freirechtle-hre)与奥地利法律社会学家艾利希(Eugen Ehrlich,1862-1922)提出了批评意见,但是他们对于"法律社会学"这门新兴的学科,却还是有不完全相同的定位。展开更多
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 ...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 AutumnWarring 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.展开更多
基金supported by the Anhui Public Welfare Geological Project(No.2015-g-25)the Special Research Project of CEA(No.TYZ20160101)
文摘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 AutumnWarring 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.
