安徽霍山戴家院遗址自然变形遗迹的发现及其特征初探
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摘要
古遗址、古墓地发掘过程中的自然变形研究是反演或充实历史和史前变形历史记录的重要工作内容之一.近期我省地震部门会同省文物考古部门,对皖西霍山戴家院考古现场进行专题发掘调查,发现了与构造运动有关的地裂缝,其中充填有砂线、砂脉.初步研究显示包括两期变形,且均显示高速变形特征,代表两次地震事件.发生时代约相当于西周晚期和春秋中晚期,前者规模较大,含砂裂缝长轴方向平行于近侧的地震活动断裂方向.本次发现及初步分析填补了东部地区西周到春秋期自然变形事件研究空白.
The stuudy of natural deformation vestige during the disentombing to the ruins and tumulus is one of the important tasks in inverting or substantiating history and prehistoric deformation records.Recently,the Earthquake Administration cooperates with department of cultural relics and archaeology to explore and investigate Daijiayuan vestige at Huoshan in western Anhui.We found the sand line and sand vein filled in the crack.It may relate with tectonic movement.It shows 2 times of tectonic deformation from the preliminary research,and it shows the characteristic with high rate.They represent 2 earthquake events.It is about equivalent to the later period of Xizhou Dynasty and in the middle-later period of Chunqiu Dynasty in era,the former is larger in scale,with the long axis direction of crack of sand parallel to the direction of the seismic fracture in the near side.This discovery and initial study is the first one about the natural deformation in East China from Xizhou Dynasty to Chunqiu Dynasty.
The stuudy of natural deformation vestige during the disentombing to the ruins and tumulus is one of the important tasks in inverting or substantiating history and prehistoric deformation records.Recently,the Earthquake Administration cooperates with department of cultural relics and archaeology to explore and investigate Daijiayuan vestige at Huoshan in western Anhui.We found the sand line and sand vein filled in the crack.It may relate with tectonic movement.It shows 2 times of tectonic deformation from the preliminary research,and it shows the characteristic with high rate.They represent 2 earthquake events.It is about equivalent to the later period of Xizhou Dynasty and in the middle-later period of Chunqiu Dynasty in era,the former is larger in scale,with the long axis direction of crack of sand parallel to the direction of the seismic fracture in the near side.This discovery and initial study is the first one about the natural deformation in East China from Xizhou Dynasty to Chunqiu Dynasty.
引文
[1] 刘颖,谢君斐,等.1984． 砂土震动液化[M].地震出版社,北京. Liu Y,Xie J F,et al.1984． Sandy soil seismic liquefaction[M].Seismological Press,Beijing.
[2] Turtle M P J,Collier L W W,Lafferty R H.New evidence for a large earthquake in the New Madrid seismic zone between A.D.1400 and 1670[J].Geology,1999,27:7771～7774．
[3] 姚大全.活动断层周期性粘滑变形的宏观和微观证据[J].国际地震动态,2004,4:6～10． Yao D Q.Macroscopic and microscopic evidence of periodical stick-slip deformation in an active fault [J].Recent Developments in Word Seismology,2004,4 :6 ～ 10．
[4] 从柏林,王清晨.大别山 苏鲁超高压变质带研究的最新进展[J].科学通报,1999,44(11) :11 27～1141． Cong B L,Wang Q C.The latest research progress on the ultrahigh-pressure metamorphic zone from the Dabie-Sulu Mountains[J].Science Bulletin,1999,44(11) :1127～1141．
[5] 杨文采,余长青.根据地球物理资料分析大别-苏鲁超高压变质带演化的运动学与动力学[J].地球物理学报,2001,44(3) :346～359． Yang W C,Yu C Q.Kinetics and dynamics of development of the Dabie-Sulu UHPM terrenes based on geophysical evidences [J].Chinese J.Geophys,2001,44(3) :346～359．
[6] 徐纪人,杨文采,赵志新,等.苏鲁大别造山带岩石圈三维P波速度结构特征[J].地质学报,2003,77(4) :577～582． Xu J R,Yang W C,Zhao Z X,et al.Three dimensional Velocity Structures of the Sulu Dabie Origin Belt[J].Acta Geological Sinica,2003,77(4) :577～582．
[7] 赵志新,徐纪人,许志琴.上地幔三维S波速度结构与大别苏鲁超高压变质带俯冲折返机制探讨[J].岩石学报,2004,20(1) :157～164． Zhao Z X,Xu J R and Xu Z Q.3-D S wave velocity structure in the upper mantle and the mechanism investigation for the ultrahigh-pressure metamorphosed belt in the Dabie-Sulu region[J].Acta Petrologic Sinica,2004,20(1) :157 ～ 164．
[8] 赵志新,徐纪人.苏鲁大别及其周围地区深部P波速度结构特征的初步分析[J].岩石学报,2005,21(2) :525～532． Zhao Z X,Xu J R.Characteristic outline of P wave velocity structure in the depth beneath the Sulu-Dabie region[J].Acta Petrologic Sinica,2005,21(2) :525～532．
[9] 肖骑彬,赵国泽,詹艳,等.大别山超高压变质带深部电性结构及其动力学意义初步研究.地球物理学报,2007,50(3) :812～822． Xiao Q B,Zhao G Z,Zhan Y,et al.A preliminary study on electrical structure and dynamics of the ultra-high pre88ure metamorphic belt beneath the Dabie Mountains[J].Chinese J.Dp.,2007,50(3) :812～822．
[10] 刘建华,刘福田.秦岭-大别造山带及其南北缘地震层析成像[J].地球物理学报,1995,38(1) :46～54． Liu J H,Liu F T.Seismic tomography velocity structure in the Qinling Dabie orogenic belt and its north and south edges [J].Chinese J.Geophys.,1995,38 ..46 ～ 54．
[11] 徐佩芬,刘福田,王清晨,等.大别 苏鲁碰撞造山带的地震成像研究--岩石圈三维速度结构[J].地球物理学报,2000,43(3) :377～385． Xu P F,Liu F T,Wang Q C,et al.Seismic tomography beneath the Dabie Sulu collision origin 3-D velocity structure of lithosphere[J].Chinese J.Geophys.,2000,43 (3) :377～385．
[12] 姚大全,刘加灿.六安-霍山地震危险区地震活动和地震构造[J].地震地质,2003,25(2) :209～219． Yao D Q,Liu J C.Seismic activities and structures of the Luan-Huoshan seismic risk area[J].Seismology and Geology,2003,25(2) :209～219．
[13] 黄玮琼,李文香,曹学峰.中国大陆地震资料完整性研究[J].地震学报,1994． 16(4) :423～432． Huang W Q,Li W X,Cao X F.Study on seismic data integrity in Chinese mainland[J].Acta Seismological Sinica,1994,16(4) :423～432．
[2] Turtle M P J,Collier L W W,Lafferty R H.New evidence for a large earthquake in the New Madrid seismic zone between A.D.1400 and 1670[J].Geology,1999,27:7771～7774．
[3] 姚大全.活动断层周期性粘滑变形的宏观和微观证据[J].国际地震动态,2004,4:6～10． Yao D Q.Macroscopic and microscopic evidence of periodical stick-slip deformation in an active fault [J].Recent Developments in Word Seismology,2004,4 :6 ～ 10．
[4] 从柏林,王清晨.大别山 苏鲁超高压变质带研究的最新进展[J].科学通报,1999,44(11) :11 27～1141． Cong B L,Wang Q C.The latest research progress on the ultrahigh-pressure metamorphic zone from the Dabie-Sulu Mountains[J].Science Bulletin,1999,44(11) :1127～1141．
[5] 杨文采,余长青.根据地球物理资料分析大别-苏鲁超高压变质带演化的运动学与动力学[J].地球物理学报,2001,44(3) :346～359． Yang W C,Yu C Q.Kinetics and dynamics of development of the Dabie-Sulu UHPM terrenes based on geophysical evidences [J].Chinese J.Geophys,2001,44(3) :346～359．
[6] 徐纪人,杨文采,赵志新,等.苏鲁大别造山带岩石圈三维P波速度结构特征[J].地质学报,2003,77(4) :577～582． Xu J R,Yang W C,Zhao Z X,et al.Three dimensional Velocity Structures of the Sulu Dabie Origin Belt[J].Acta Geological Sinica,2003,77(4) :577～582．
[7] 赵志新,徐纪人,许志琴.上地幔三维S波速度结构与大别苏鲁超高压变质带俯冲折返机制探讨[J].岩石学报,2004,20(1) :157～164． Zhao Z X,Xu J R and Xu Z Q.3-D S wave velocity structure in the upper mantle and the mechanism investigation for the ultrahigh-pressure metamorphosed belt in the Dabie-Sulu region[J].Acta Petrologic Sinica,2004,20(1) :157 ～ 164．
[8] 赵志新,徐纪人.苏鲁大别及其周围地区深部P波速度结构特征的初步分析[J].岩石学报,2005,21(2) :525～532． Zhao Z X,Xu J R.Characteristic outline of P wave velocity structure in the depth beneath the Sulu-Dabie region[J].Acta Petrologic Sinica,2005,21(2) :525～532．
[9] 肖骑彬,赵国泽,詹艳,等.大别山超高压变质带深部电性结构及其动力学意义初步研究.地球物理学报,2007,50(3) :812～822． Xiao Q B,Zhao G Z,Zhan Y,et al.A preliminary study on electrical structure and dynamics of the ultra-high pre88ure metamorphic belt beneath the Dabie Mountains[J].Chinese J.Dp.,2007,50(3) :812～822．
[10] 刘建华,刘福田.秦岭-大别造山带及其南北缘地震层析成像[J].地球物理学报,1995,38(1) :46～54． Liu J H,Liu F T.Seismic tomography velocity structure in the Qinling Dabie orogenic belt and its north and south edges [J].Chinese J.Geophys.,1995,38 ..46 ～ 54．
[11] 徐佩芬,刘福田,王清晨,等.大别 苏鲁碰撞造山带的地震成像研究--岩石圈三维速度结构[J].地球物理学报,2000,43(3) :377～385． Xu P F,Liu F T,Wang Q C,et al.Seismic tomography beneath the Dabie Sulu collision origin 3-D velocity structure of lithosphere[J].Chinese J.Geophys.,2000,43 (3) :377～385．
[12] 姚大全,刘加灿.六安-霍山地震危险区地震活动和地震构造[J].地震地质,2003,25(2) :209～219． Yao D Q,Liu J C.Seismic activities and structures of the Luan-Huoshan seismic risk area[J].Seismology and Geology,2003,25(2) :209～219．
[13] 黄玮琼,李文香,曹学峰.中国大陆地震资料完整性研究[J].地震学报,1994． 16(4) :423～432． Huang W Q,Li W X,Cao X F.Study on seismic data integrity in Chinese mainland[J].Acta Seismological Sinica,1994,16(4) :423～432．
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