1812年尼勒克地震断层及最大位移
|
摘要
通过野外考察和地貌变形测量等手段,研究了尼勒克1812年8级地震的地震断层的平面分组特点、活动性质、分段特征,讨论了地震滑塌构造、地震断层与重力滑坡的区别,分析了线性滑坡后壁与地震断层的潜在关系。在正确区分地震断层和滑坡后壁的基础上,确定了地震断层的最大位移。该形变带从吉仁台延伸到乔尔马以东,东西总长124 km,南北最宽处约28 km,地震断层断续展布97 km,最大垂直错距为15 m,水平位移为4 m。
Through using methods of several field inspecting and topographical deformation measuring,we studied plane distribution,activity and subsection characteristic of the fault of Nileke earthquake in 1812.And discussed difference of seismic slacktip structure,earthquake fault and gravity slide.And analyzed the latency relation between linearity coast back wall and earthquake fault.Based on accurate division with seismic fault and coast back wall,the maximal displacement is confirmed.The results show that the total length of the deformation zone in EW from Jiren station to east of Mayibulake is 124 km,the width of the deformation zone in NS is about 28 km,its length of distributing of the intermittently fault is 97 km,the maximal uprightness dislocation of the earthquake fault is 15 m,and the level displacement is 4 m.
Through using methods of several field inspecting and topographical deformation measuring,we studied plane distribution,activity and subsection characteristic of the fault of Nileke earthquake in 1812.And discussed difference of seismic slacktip structure,earthquake fault and gravity slide.And analyzed the latency relation between linearity coast back wall and earthquake fault.Based on accurate division with seismic fault and coast back wall,the maximal displacement is confirmed.The results show that the total length of the deformation zone in EW from Jiren station to east of Mayibulake is 124 km,the width of the deformation zone in NS is about 28 km,its length of distributing of the intermittently fault is 97 km,the maximal uprightness dislocation of the earthquake fault is 15 m,and the level displacement is 4 m.
引文
[1]国家地震局震害防御司.中国历史强震目录[M].北京:地震出版社,1995.
[2]新疆维吾尔自治区地震局.地震资料汇编[G].北京:地震出版社,1985.
[3]杨章,陈祥玉,尹光华,等.1812年3月8日新疆尼勒克8级大震[J].西北地震学报,1985,7(1):59-65.
[4]冯先岳.新疆尼勒克地震断层带[J].内陆地震,1990,4(3):273-277.
[5]Wallace R E.Profiles and Ages of Young Fault Scarps in North-central Nevada[J].Geological Society of America Bulletin,1977,88(9):1 267-1 281.
[6]Buknam R C,Anderson R E.Estimstion of fault scarp ages from a scarp-jeoght-slope-angle relationship[J].Geology,1979.7(1):11-14.
[7]尹光华.新疆伊犁盆地新构造运动与地震[J].内陆地震,1993,7(2):180-187.
[8]刘百篪,周俊喜,李秦梅,等.1718年通谓地震和1654年天水地震区航空照片判读[J].地震科学研究,1984,6(1):56-67.
[9]尹光华,买颜东,蒋伯军,等.新疆独山子GPS形变测量与断层活动性研究[J].内陆地震,1999,13(4):345-351.
[10]尹光华,李军,张勇,等.尼勒克地震滑坡的统计分析及初步研究[J].内陆地震,2001,15(1):56-63.
[11]冯先岳.新疆古地震[M].乌鲁木齐:新疆科技卫生出版社,1997.
[12]尹光华,蒋靖祥,张勇,等.1812年尼勒克大地震的地表破坏[C]//李克,王兰民,刘耀炜.中国八级大震研究及防震减灾学术会议论文集.北京:地震出版社,2001:31-37.
[13]朱海之.我国黄土地区地震崩滑灾害的研究[M]//国家地震局地质研究所.现代地壳运动研究.北京:地震出版社.1987:165-175.
[14]尹光华,蒋靖祥,张勇,等.新疆尼勒克1812年地震断层构造特征[J].西北地震学报,2002,24(2):183-186.
[15]尹光华,蒋靖祥,张勇.新疆伊犁喀什河断裂及其活动性研究[J].内陆地震,2003,17(2):109-116.
[2]新疆维吾尔自治区地震局.地震资料汇编[G].北京:地震出版社,1985.
[3]杨章,陈祥玉,尹光华,等.1812年3月8日新疆尼勒克8级大震[J].西北地震学报,1985,7(1):59-65.
[4]冯先岳.新疆尼勒克地震断层带[J].内陆地震,1990,4(3):273-277.
[5]Wallace R E.Profiles and Ages of Young Fault Scarps in North-central Nevada[J].Geological Society of America Bulletin,1977,88(9):1 267-1 281.
[6]Buknam R C,Anderson R E.Estimstion of fault scarp ages from a scarp-jeoght-slope-angle relationship[J].Geology,1979.7(1):11-14.
[7]尹光华.新疆伊犁盆地新构造运动与地震[J].内陆地震,1993,7(2):180-187.
[8]刘百篪,周俊喜,李秦梅,等.1718年通谓地震和1654年天水地震区航空照片判读[J].地震科学研究,1984,6(1):56-67.
[9]尹光华,买颜东,蒋伯军,等.新疆独山子GPS形变测量与断层活动性研究[J].内陆地震,1999,13(4):345-351.
[10]尹光华,李军,张勇,等.尼勒克地震滑坡的统计分析及初步研究[J].内陆地震,2001,15(1):56-63.
[11]冯先岳.新疆古地震[M].乌鲁木齐:新疆科技卫生出版社,1997.
[12]尹光华,蒋靖祥,张勇,等.1812年尼勒克大地震的地表破坏[C]//李克,王兰民,刘耀炜.中国八级大震研究及防震减灾学术会议论文集.北京:地震出版社,2001:31-37.
[13]朱海之.我国黄土地区地震崩滑灾害的研究[M]//国家地震局地质研究所.现代地壳运动研究.北京:地震出版社.1987:165-175.
[14]尹光华,蒋靖祥,张勇,等.新疆尼勒克1812年地震断层构造特征[J].西北地震学报,2002,24(2):183-186.
[15]尹光华,蒋靖祥,张勇.新疆伊犁喀什河断裂及其活动性研究[J].内陆地震,2003,17(2):109-116.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心