河南平顶山平煤矿区天然地震、爆破、塌陷时频特征分析     

高家乙  刘晓锋  闫睿 《地震地磁观测与研究》2020,41(3):67-74

选取2019年3月—8月河南平顶山市宝丰县平煤矿区发生的ML 2.0—2.9天然地震、爆破、塌陷等9次震动事件,在区域地质构造背景和波形特征分析基础上,采用短时傅里叶变换(STFT)方法开展时频波谱分析,提取不同类型事件的时频特征。结果显示:(1)天然地震频率成分丰富,且高、低频分布均匀,P波在约3 Hz和8 Hz处存在2个峰值,S波存在多个峰值;(2)爆破事件的时频谱相对集中,以低频为主,P波频率峰值约5Hz,信号主频随时间变化,大致呈线性降低至1—2 Hz;(3)塌陷事件频率成分以4 Hz以下的低频为主,P波无明显峰值且频率成分单一,主频出现在2 Hz左右的面波。本文结果可为今后该矿区震动事件类型判断提供参考依据。  相似文献   

走向21世纪的地壳形变学--对大陆动力学与地震预测的新推动   总被引：2，自引：2，他引：0  

周硕愚 《大地测量与地球动力学》1999,19(1):1-13

监测和预测地震等自然灾害的需要,促进了大地测量学和地球物理学等学科的相互交融.经过30余年的探索,一门地学前沿交叉新学科--"地壳形变学"已初步形成.地壳形变学已拥有空间-地面-深部立体测地系统,具有在多种空间尺度内精确测定现今地壳运动(秒～数十年)和灾害孕育过程的空前强大能力,从而可望击破长期制约现今地球动力学和地震预测的地球空间信息的"瓶颈".在21世纪,地壳形变学将成为推动大陆动力学和地震预报的主要科技动力之一,推进精确定量测定大陆动力学现今过程,限定现今大陆动力学性质并在验证解释地质学模型诸方面发挥特有作用.它将促使地震预测摆脱"粘滞状态",由"经验预测"走向"图像动力学预测";在揭示大陆地震孕育时空过程、判定地震大形势、划定危险区、搜寻和跟踪震源动力学演化过程及研究动力学响应耦合等方面作出新贡献.  相似文献   

90年代我国区域经济合作政策效果分析   总被引：18，自引：5，他引：13  

庞效民 《地理研究》1999,18(3):231-240

通过对90年代以来我国区域经济合作的具体实践进行总结和分析,论证分析我国推动地区经济技术合作政策的合理性和可行性。作者从明确中央政府和地方政府有关地区经济技术合作以及区域经济合作的政策目标出发,深入分析区域合作组织的合作动力机制及其实际进展,对区域经济合作取得的成果与当前区域合作中遇到的障碍和问题进行客观评价,并在此基础上提出有关政策建议。提出区域合作组织的发展只能对中央政府推动地区合作战略目标的实现作局部性贡献;总体而言,我国政府通过提倡地区经济技术合作来解决区域问题的国家地区协调发展战略目标的实现在一定阶段内缺少现实合理性。  相似文献   

A relationship between solar activity and frequency of natural disasters in China   总被引：2，自引：0，他引：2  

WANG Zhongrui  Song FENG  TANG Maocang 《大气科学进展》2003,20(6):934-939

The relationship between the length of the solar cycle, a good indicator of long-term change in solar activity, and natural disasters (drought, flood, and strong earthquakes) in China during the last 108 years is analyzed. The results suggest that the length of solar cycle may be a useful indicator for drought/flood and strong earthquakes. When the solar activity strengthens, we see the length of the solar cycle shorten and more floods occur in South China and frequent strong earthquakes happen in the Tibetan Plateau,but the droughts in East China as well as the strong earthquakes in Taiwan and at the western boundary of China are very few. The opposite frequencies occur when the solar activity weakens. The current study indicates that the solar activity may play an important role in the climate extremes and behavior in the lithosphere.  相似文献   

Automatic Location of Swarm Earthquakes from Local Network Data     

Fischer  Tomáš 《Studia Geophysica et Geodaetica》2003,47(1):83-98

An advanced method of automated seismic phase picking and exact location and magnitude determination of swarm micro-earthquakes from local network data is presented. The phase picker is applied in two steps: first, S-wave groups are identified using a polarisation detector, and then corresponding P-wave groups are searched for. The times of maximum P- and S-amplitudes are then used as starting points for the determination of accurate P- and S-arrival times. The maximum S-wave amplitudes are utilised for determining local magnitudes. The whole procedure is checked by simultaneous preliminary hypocentre location providing estimates of local magnitudes and a compatibility check of the candidate P- and S-phases. The closest station to the earthquake cluster is used as a master, and the phase search at the remaining stations is governed by the P- and S-phases identified at the master station. Thanks to the use of apriori information on the approximate position of hypocentres, the procedure is also capable of picking the individual P- and S-phases of sequences of overlapping swarm events. The performance of the procedure was tested by comparison of the automatically and interactively created catalogues of the January 1997 NW-Bohemia micro-earthquake swarm. With stations located at epicentral distances between 0 and 20 km, the difference between hypocentre coordinates obtained by automatic and interactive processing did not exceed 80 m for 86% events. All events above magnitude 0.5 were identified, and the automatically determined polarity of first P-wave motion proved to be correct in 89% of them.  相似文献   

昆仑山口西8.1级地震前的地震活动异常及预测意义的讨论   总被引：2，自引：0，他引：2       下载免费PDF全文

王林瑛  陈佩燕  林碧苍  丁秋琴 《地震工程学报》2003,25(1):22-27

昆仑山口西8．1地震前明显地出现大区域地震活动平静、高6值、高调制、低锅值的异常配套现象．回顾性分析了巨大地震前不同时问和空间尺度的地震活动性异常,探讨了巨大地震的预测可能性。  相似文献   

昆仑山口西8.1级地震后青藏高原北部地区地震活动初步研究   总被引：11，自引：4，他引：7       下载免费PDF全文

刘小凤  杨立明  范兵 《地震工程学报》2003,25(1):52-58

利用相关震例分析了昆仑山口西8．1级地震后青藏高原北部地区未来1～3年地震活动特征．结果表明,沿东昆仑构造带及邻近地区发生Ms≥7．0地震后青藏高原北部地区中强地震活动有增强的趋势,祁连山地震带和东昆仑地震带的地震活动具有交替发生的特征,未来1～3年中强地震主体活动区为大型走滑活动断裂上应力转换部位和挤压会聚构造区,如东昆仑断裂带中东段和祁连山地震带中东段和西段。  相似文献   

地震速报参数不确定性的应急灾害损失快速评估模型   总被引：7，自引：0，他引：7  

王晓青  邵辉成  丁香 《地震工程与工程振动》2003,23(6):198-201

本文针对目前地震应急灾害损失快速评估中存在的问题,建立了考虑地震速报参数不确定性的灾害损失快速评估模型。并利用1990年来全国的81组速报震中与宏观震中数据。得到速报震中与宏观震中偏差的概率分布经验参数。  相似文献   

新疆伽师强震群强震主破裂面走向初探   总被引：7，自引：2，他引：5       下载免费PDF全文

苏廼秦 《地震工程学报》2003,25(3):269-274

1997年1月21日-1998年8月27日新疆伽师发生了包含9次6级地震的强震群,震源机制解表明有NE向和NW向两个节面．有观点认为主破裂面为NNW向．本通过数字地震台阵的余震序列精确定位、震源破裂过程及滑动方向、震群空间分布图像、地震烈度等震线长轴走向和微、宏观震中动态变化方向等多种方法分析后,综合判定9次6级地震的主破裂面走向极可能为北东方向．  相似文献   

Multi‐variable relations for soil effects on seismic ground motion     

George D. Bouckovalas  Achilleas G. Papadimitriou 《地震工程与结构动力学》2003,32(12):1867-1896

Soil effects on peak ground acceleration, velocity and elastic response spectra (5% damping) are expressed by simple approximate relations in terms of five key parameters: (a) the fundamental vibration period of the non‐linear soil, T_S, (b) the period of a bedrock site of equal thickness, T_b, (c) the predominant excitation period, Te, (d) the peak seismic acceleration at outcropping bedrock, a, and (e) the number of significant excitation cycles, n. Furthermore, another relation is proposed for the estimation of T_S in terms of the soil thickness H, the average shear wave velocity of the soil V?_S,o and a. The aforementioned parameters were first identified through a simplified analytical simulation of the site excitation. The multivariable approximate relations were then formulated via a statistical analysis of relevant data from more than 700 one‐dimensional equivalent‐linear seismic ground response analyses, for actual seismic excitations and natural soil conditions. Use of these relations to back‐calculate the numerical results in the database gives an estimate of their error margin, which is found to be relatively small and unbiased. The proposed relations are also independently verified through a detailed comparison with strong motion recordings from seven well‐documented case studies: (a) two sites in the San Fernando valley during the Northridge earthquake, and (b) five different seismic events recorded at the SMART‐1 accelerometer array in Taiwan. It is deduced that the accuracy of the relations is comparable to that of the equivalent‐linear method. Hence, they can be readily used as a quick alternative for routine applications, as well as for spreadsheet computations (e.g. GIS‐aided seismic microzonation studies) where numerical methods are cumbersome to implement. Copyright © 2003 John Wiley & Sons, Ltd.  相似文献