2003年岷县5.5级地震地震学前兆特征及预报意义          下载免费PDF全文

李亚荣  荣代潞  韩晓明 《地震工程学报》2007,29(2):150-155

研究了2003年甘肃岷县5.5级地震的地震学前兆的变化特征,显示尾波Qc值和地震空间相关长度在震前都呈增长趋势,用幂次率关系对这种变化进行了拟合。结果为利用尾波Q值和地震空间相关长度的监测资料建立预测地震发生时间的方法和指标打下了基础。  相似文献   

Attenuation of Coda Waves at the Changbaishan Tianchi Volcanic Area in Northeast China   总被引：2，自引：0，他引：2  

Jianping Wu  Wenjie Jiao  Yuehong Ming  Wei Su 《Pure and Applied Geophysics》2006,163(7):1351-1368

21 earthquakes recorded by a temporary seismic network in the Changbaishan Tianchi volcanic area in Northeast China operated during the summer of 2002 and 2003 were analyzed to estimate the S coda attenuation. The attenuation quality factor Q_c was estimated using the single scattering attenuation model of Sato (1977) in the frequency band from 4 to 24 Hz. All the events studied in this paper occurred at depths from 2 to 6 km with ML of 1.4–2.8. The epicentral distances are less than 25 km. For all events which occurred near the Tianchi Lake (caldera), the Q_c patterns obtained at the stations near the lake are similar, and the Q_c values are relatively small. At the stations located about 15 km east of the Tianchi Lake, however, the average Q_c is significantly higher. For an event which occurred 25km from the lake to the west, Q_c patterns derived at the stations near the lake are quite similar to the above mentioned Q_c for stations located in the east. Further study shows that Q_c value in the north and central areas of the volcano is relatively lower than that in the surrounding area. Compared to other volcanic areas in the world, the average Q_c of the Changbaishan Tianchi volcanic area is obviously lower. The deep seismic sounding and teleseismic receiver function studies indicated more than one lower velocity layer in the crust. The MT studies suggested the presence of high conductive bodies beneath the area. We interpret the strong attenuation of coda waves near the Changbaishan Tianchi volcano as being possibly related to high temperature medium caused by shallow magma chambers.  相似文献   

岫岩5.4级地震前后尾波振动持续时间比的演化特征   总被引：1，自引：0，他引：1  

曹凤娟  孙文福  李芳  于龙伟  于笑非 《东北地震研究》2003,19(3):18-23

本文在前人工作的基础上，从地震波的动力学特性出发，利用尾波振动持续时间比τH/τv方法，对1999年11月29日岫岩Ms5．4地震前后地震活动的演化特征进行了详细研究。结果发现在岫岩Ms5．4地震前，距震中相对较近台站记录到的尾波振动持续时间比一rH／TV存在一定程度的异常显示，而距震中较远外围地区的台站记录到的一τH／τv震前无明显的异常反应。认为尾波振动持续时间比τH／τv从统计意义上提供了研究介质物理性质的较好方法，对短临地震预报具有一定的参考意义。  相似文献   

Determination of first mode ground period and site-dependent design response spectrum for Taiwan High Speed Rail     

Juin-Fu Chai  Tsung-Jen Teng  Chin-Hsiung Loh 《Soil Dynamics and Earthquake Engineering》2004,24(7):527-536

The objective of this paper is to identify the first mode ground period T_g, at each interesting site along Taiwan High Speed Rail (THSR) route, and further, to determine the site-dependent design response spectrum for particular sites with T_g larger than 1 s. In this paper, a linear model of shear wave propagating in a multi-layered half-space is developed to identify the first mode ground period T_g of an interesting site on the basis of the field bore hole data. Furthermore, for each one of the strong ground motion observation stations within the Chiayi-Tainan area, the first mode ground period T_g was identified by either coda waves or pre-event ambient vibrations from the seismograms. In addition, the site-specific parameter C_v in defining the normalized response spectrum was also determined based on the observed strong ground motions at the specified observation station, and hence the empirical function between T_g and C_v can be regressed for this interesting area. Therefore, for a particular site along THSR route within the Chiayi-Tainan area, the site-specific parameter C_v can be determined from the regressed empirical function by the identified first mode ground period T_g, and further, used to develop the site-dependent design response spectrum.  相似文献   

江苏地区尾波Q值特征研究     

孙业君  黄耘  王斌  王俊  李锋  江昊琳 《中国地震研究》2014,28(2):188-199

基于Aki单次散射模型,利用江苏数字地震台网记录的地震数字波形资料开展了江苏地区尾波Q值特征研究。结果表明,江苏地区总体上属于高Q值地区,但不同地区存在明显差异,总体呈现出南高北低的特点。本文对台站相对密,地质构造特点明显、尾波Q0计算结果较为集中的四个区域分区进行了研究,获得了江苏四个区域的Q值与频率的特征关系。苏南至长江口和茅山断裂带附近为江苏的高Q值地区,苏中至沿岸为江苏的低Q值地区,苏北连云港及附近处于Q值中等水平地区。对照江苏四个Q值不同分区的构造及地震活动分析,Q值、地壳运动和地震活动性之间存在一定的相关关系。  相似文献   

2013年吉林前郭5.8级震群地震序列尾波Q值研究     

张洪艳  康建红  卢燕红  张宇  陈聪 《华北地震科学》2014,(3):10-14

挑选出2013年10月31日至12月31日前郭地区发生的58次M1.0以上地震事件,基于Sato的单次散射模型分别计算了长岭台、松原台和乾安台的尾波Q值,获得了3个台尾波Q值与频率的依赖关系,分别为：Qc=33.65f^0.9782、Qc=33.00f^0.9104、Qc=33.46f^1.0299。初步认为研究区内的Q值在2~18Hz范围内与频率有显著的相关性,研究区内的低Q值现象与该区地质构造、地震活动性形成了较好的一致性。  相似文献   

紫坪铺水库地区尾波Q_C值研究   总被引：1，自引：0，他引：1  

周连庆  赵翠萍  陈章立 《地震》2009,29(4)

利用Sato模型研究了汶川 M_S8.0地震前位于震源区的紫坪铺水库地区尾波 Q_C值特征. 结果表明,库区 Q_C值与频率有很强的依赖关系,4个台站的平均 Q_C=21.6 f~(1.211),尾波 Q_0值较小,平均为21.6. 离震群最近的MZP台 Q_0最大,为29.0,离震群最远的BAJ台 Q_0最小,为13.9. 这种尾波 Q_0值的差别可能与尾波 Q 值所反映的介质深度存在一定的关系,而较小的流逝时间可能是这里η值偏高的原因之一.  相似文献   

Attenuation of coda waves in the Northeastern Region of India   总被引：1，自引：0，他引：1  

Devajit Hazarika  Saurabh Baruah  Naba Kumar Gogoi 《Journal of Seismology》2009,13(1):141-160

Coda wave attenuation quality factor Qc is estimated in the northeastern region of India using 45 local earthquakes recorded by regional seismic network. The quality factor Qc was estimated using the single backscattering model modified by Sato (J Phys Earth 25:27–41, 1977), in the frequency range 1–18 Hz. The attenuation and frequency dependence for different paths and the correlation of the results with geotectonics of the region are described in this paper. A total of 3,890 Qc measurements covering 187 varying paths are made for different lapse time window of 20, 30, 40, 50, 60, 70, 80, and 90 s in coda wave. The magnitudes of the analyzed events range from 1.2 to 3.9 and focal depths range between 7 and 38 km. The source–receiver distances of the selected events range between 16 and 270 km. For 30-s duration, the mean values of the estimated Qc vary from 50 ± 12 (at 1 Hz) to 2,078 ± 211(at 18 Hz) for the Arunachal Himalaya, 49 ± 14 (at 1 Hz) to 2,466 ± 197 (at 18 Hz) for the Indo-Burman, and 45 ± 13 (at 1 Hz) to 2,069 ± 198 (at 18 Hz) for Shillong group of earthquakes. It is observed that Qc increases with frequency portraying an average attenuation relation for the region. Moreover, the pattern of Qc^− 1 with frequency is analogous to the estimates obtained in other tectonic areas in the world, except with the observation that the Qc^− 1 is much higher at 1 Hz for the northeastern region. The Qc^− 1 is about 10^− 1.8 at 1 Hz and decreases to about 10^− 3.6 at 18 Hz indicating clear frequency dependence. Pertaining to the spatial distribution of Qc values, Mikir Hills and western part of Shillong Plateau are characterized by lower attenuation.  相似文献