宁波台动水位与垂直摆对印尼8.9和日本9.0级地震的同震响应
|
摘要
分析认为宁波台ZK03井动水位与VS垂直摆倾斜仪出现的异常可能是印尼8.9和日本9.0级地震的同震响应。印尼8.9级地震后,动水位表现为地震波引起的脉冲和阶跃变化并抬高水位。垂直摆表现为形变波引起的脉冲和阶跃变化,EW向最大幅度约为408.328×10-3〃的脉冲式向E振荡波,并向W出现阶跃变化;NS向最大幅度约为295.192×10-3〃的脉冲式向N振荡波,并产生向N阶跃变化。日本9.0级地震后,动水位表现为地震波引起的脉冲和阶跃变化,10余小时后水位恢复到震前水平,垂直摆表现为形变波引起的脉冲式反复振荡变化,EW向最大幅度约为304.163×10-3〃的脉冲式向E振荡波;NS向最大幅度约为372.252×10-3〃的脉冲式向N振荡波。分析结果说明,该台垂直摆记录的形变波两分向振幅比明显不同,具有一定的方向性,即近垂直于震中分向的振幅大于近平行分向。动水位和垂直摆记录的正常固体潮形态和异常变化具有相似性。
Based on analyses of the anomalies in dynamic water level and vertical pendulum tiltmeter at the well no.ZK03 of Ningbo station,the anomalies were known as co-seismic responses of the Sumatra M8.9 earthquake and the Japan M9.0 earthquake.For the Sumatra M8.9 earthquake,the dynamic water level showed co-seismic pulse and step change to high level;the vertical pendulum showed pulse and step change caused by crustal deformation wave,the amplitude of pulse was about 408.328×10-3〃from west to east in WE direction and the step change was from east to west;the amplitude in NS direction was about 295.192×10-3〃from south to north and the step change was from south to north.After the Japan M9.0 earthquake,the dynamic water level showed pulse and step change caused by seismic wave,and recovered to the level before the earthquake after 10 hours;The vertical pendulum showed repeating pulses and the amplitude in WE direction was about 304.163×10-3〃from west to east;and the amplitude in NS direction was about 372.252×10-3〃from south to north.from the above analyses it concludes that the amplitudes of this station in the two directions were obviously different,they showed a direction sense,i.e.,the amplitude perpendicular to the earthquake focus was greater than that parallel to the earthquake focus.The normal tidal changes and the anomalous changes for dynamic water level and vertical pendulum were similar.
Based on analyses of the anomalies in dynamic water level and vertical pendulum tiltmeter at the well no.ZK03 of Ningbo station,the anomalies were known as co-seismic responses of the Sumatra M8.9 earthquake and the Japan M9.0 earthquake.For the Sumatra M8.9 earthquake,the dynamic water level showed co-seismic pulse and step change to high level;the vertical pendulum showed pulse and step change caused by crustal deformation wave,the amplitude of pulse was about 408.328×10-3〃from west to east in WE direction and the step change was from east to west;the amplitude in NS direction was about 295.192×10-3〃from south to north and the step change was from south to north.After the Japan M9.0 earthquake,the dynamic water level showed pulse and step change caused by seismic wave,and recovered to the level before the earthquake after 10 hours;The vertical pendulum showed repeating pulses and the amplitude in WE direction was about 304.163×10-3〃from west to east;and the amplitude in NS direction was about 372.252×10-3〃from south to north.from the above analyses it concludes that the amplitudes of this station in the two directions were obviously different,they showed a direction sense,i.e.,the amplitude perpendicular to the earthquake focus was greater than that parallel to the earthquake focus.The normal tidal changes and the anomalous changes for dynamic water level and vertical pendulum were similar.
引文
[1]郑江蓉,徐桂明,李鸿宇,等.2004年12月26日印尼8.7级强震后江苏地区同震效应分析.防灾减灾工程学报,2005,25(1):105-113
[2]张素欣,张子广,张跃刚,等.2004年12月26日印尼大强震河北省数字水位、地热记震能力分析.华北地震科学,2005,23(3):27-30
[3]高小其,陈华静,杨又陵,等.2004年12月26日印尼8.7级强震新疆地区的同震效应.地震地磁观测与研究,2006,27(3):40-46
[4]万永芳,叶东华,杨向东.2004年12月26日印尼8.7级强震广东地区同震效应分析.华南地震,2006,26(4):67-73
[5]张双凤,孙晴,于伟.印尼8.7级强震在河北省的震后效应初探.华北地震科学,2007,25(3):15-19
[6]张清秀,陈小云,陈莹,等.福建省数字化水位水温资料的远场效应研究.华北地震科学,2007,25(4):49-54
[7]中国地震局监测预报司.2004年印度尼西亚苏门答腊8.7级大地震及其对中国大陆地区的影响.北京:地震出版社,2005
[8]刘耀炜,陈华静,车用太.我国地震地下流体观测研究40年发展与展望.国际地震动态,2006(7):3-12
[9]夏超德.宁波地震台地倾斜模拟与数字观测对比分析.华南地震,2005,25(2):80-87
[10]邱永平.宁波地震台动水位与垂直摆对汶川8.0级地震的同震变化.华北地震科学,2009,27(1):30-33
[2]张素欣,张子广,张跃刚,等.2004年12月26日印尼大强震河北省数字水位、地热记震能力分析.华北地震科学,2005,23(3):27-30
[3]高小其,陈华静,杨又陵,等.2004年12月26日印尼8.7级强震新疆地区的同震效应.地震地磁观测与研究,2006,27(3):40-46
[4]万永芳,叶东华,杨向东.2004年12月26日印尼8.7级强震广东地区同震效应分析.华南地震,2006,26(4):67-73
[5]张双凤,孙晴,于伟.印尼8.7级强震在河北省的震后效应初探.华北地震科学,2007,25(3):15-19
[6]张清秀,陈小云,陈莹,等.福建省数字化水位水温资料的远场效应研究.华北地震科学,2007,25(4):49-54
[7]中国地震局监测预报司.2004年印度尼西亚苏门答腊8.7级大地震及其对中国大陆地区的影响.北京:地震出版社,2005
[8]刘耀炜,陈华静,车用太.我国地震地下流体观测研究40年发展与展望.国际地震动态,2006(7):3-12
[9]夏超德.宁波地震台地倾斜模拟与数字观测对比分析.华南地震,2005,25(2):80-87
[10]邱永平.宁波地震台动水位与垂直摆对汶川8.0级地震的同震变化.华北地震科学,2009,27(1):30-33
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