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德令哈地震台测震干扰频谱特征及背景分析 被引量:2
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作者 姚家骏 文勇 +4 位作者 孟鑫 陈玉华 杨立明 赵燕杰 李瑞明 《地震地磁观测与研究》 2011年第6期28-34,共7页
通过3个台站地脉动频谱特征的对比,发现德令哈地震台地脉动记录6.5—7.5 Hz频段存在明显的高频干扰。根据2008年1月至2010年10月以来该高频干扰的频谱演化规律,对其产生背景来源做初步分析,在一定程度上解释了德令哈地震台P波记录个数... 通过3个台站地脉动频谱特征的对比,发现德令哈地震台地脉动记录6.5—7.5 Hz频段存在明显的高频干扰。根据2008年1月至2010年10月以来该高频干扰的频谱演化规律,对其产生背景来源做初步分析,在一定程度上解释了德令哈地震台P波记录个数减少的原因。 展开更多
关键词 测震环境 高频干扰 频谱特征
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Three-dimensional Building Damage Simulation Based on GIS
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作者 Gu Guoliang Jiang Lixin 《Earthquake Research in China》 2012年第4期520-531,共12页
GIS technology has been applied to building damage analysis around the world. However, most previous studies focused on the application of 2-D GIS technology, and the results from traditional earthquake damage predict... GIS technology has been applied to building damage analysis around the world. However, most previous studies focused on the application of 2-D GIS technology, and the results from traditional earthquake damage prediction are displayed in 2-D figures and charts, which is incapable of demonstrating the 3-D spatial characteristics of buildings. Taking brick-concrete building as an example, we study the characteristics of building damage, and effectively combine the information of building textures and earthquake damage. Then, we apply Google SketchUp techniques to create building models and display them with seismic damage texture in the ArcGIS Engine software development environment. In this paper we propose a solid idea for 3-D simulation of earthquake damage, which is helpful in earthquake damage prediction, virtual emergency rescue practice and earthquake knowledge education. 展开更多
关键词 Google SketchUp 3-D GIS Earthquake damage prediction Earthquake damage simulation
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Features of the M7.9 Earthquake in the Russia-Mongolia-China Boundary Region
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作者 RouJie YangYouling SongHeping 《Earthquake Research in China》 2004年第4期357-364,共8页
At 19:33 p.m on September 27, 2003, an earthquake with M7.9 occurred in the Russia-Mongolia-China boundary Region. It was strongly felt in the Altay region of Xinjiang. The losses caused by the earthquake was 76 milli... At 19:33 p.m on September 27, 2003, an earthquake with M7.9 occurred in the Russia-Mongolia-China boundary Region. It was strongly felt in the Altay region of Xinjiang. The losses caused by the earthquake was 76 million yuan (RMB). Some information about the earthquake was outlined, including basic parameters, focal mechanism, evaluation of earthquake disaster losses and so on. The satellite remote sensing information worked initial analysis for deformation of ground and failure phenomenon. 展开更多
关键词 Russia-Mongolia-China boundary region The M7.9 earthquake Focal mechanism Remote sensing Seismotectonic environment
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Processing Seismic Ambient Noise Data to Obtain Reliable Surface Wave Dispersion Measurements
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作者 Li Lingli Wang Weitao +4 位作者 Zhu Liangbao Chen Haopeng Wang Qingdong Miao Peng Wang Jun 《Earthquake Research in China》 CSCD 2015年第2期214-224,共11页
Ambient noise tomography is a rapidly emerging field of seismological research. This paper presents the current status of ambient noise data processing and its development history over the past several years, with the... Ambient noise tomography is a rapidly emerging field of seismological research. This paper presents the current status of ambient noise data processing and its development history over the past several years, with the intention to explain and justify this development through salient examples. The ambient noise data processing procedure can be divided into four principal phases: ① single station data preparation; ② cross- correlation and temporal stacking; ③ measurements of dispersion curves ( performed with frequency-time analysis for both group and phase speeds) ; ④ quality control, including SNR analysis and selection of the acceptable measurements. In addition, we provide a specific solution for a better use of the seismic station data to ambient noise study. 展开更多
关键词 Seismic ambient noise Cross-correlation Rayleigh surface wave Dispersion curves
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Mining-Induced Seismicity in the Kola Peninsula Mines
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作者 Anatoly Kozyrev Viktor Panin Iuliia Fedotova 《Journal of Civil Engineering and Architecture》 2013年第7期897-906,共10页
Mining-induced seismicity is a reflection of rock geomechanical evolution of geological environment in the natural and man-made systems and in the mining-technical systems. In order to predict and prevent mining-induc... Mining-induced seismicity is a reflection of rock geomechanical evolution of geological environment in the natural and man-made systems and in the mining-technical systems. In order to predict and prevent mining-induced seismicity, it is necessary to research geodynamics and stress state of intact rock mass, to determine possible deformations and additional stresses as a result of large-scale rock extraction, conditions of accumulated energy release. For that a geodynamical monitoring is required on every stage of deposit development and a closing. The report considers principal influencing factors of preparation and occurrence of mining-induced earthquakes. Also it estimates precursors and indicators of rock mass breaking point, and experience concerning prediction and prevention of mining-induced seismicity in the Khibiny apatite mines in the Murmansk region, which is the largest mining province. 展开更多
关键词 Mining-induced seismicity PREDICTION precursors large-scale rock extraction.
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