山西中部地区农村民居震害特征及抗震对策   总被引：1，自引：0，他引：1  

武玉柱 《山西地震》2006,(2):12-15

收集整理山西中部地区历史地震灾害资料,总结了山西中部地区农村民居由地震引起的地基震害、建筑结构震害、建筑材料与施工震害三大特征,讨论了今后农村民居和村镇公共建筑的抗震对策。为将地震造成的民居震害损失降到最低程度,提出要实行总体规划,增强防震减灾意识,加强对农村民居抗震工作的指导的建议。  相似文献   

Characteristics of coda wave attenuation in Yunnan area     

王伟君  刘杰陈凌 《地震学报(英文版)》2006,19(1):8-19

The characteristic of seismic coda wave attenuation in Yunnan area in 7 frequency-bands range from 1 Hz to 20 Hz was estimated by using the local earthquake's waveform data recorded from 22 Yunnan digital seismic stations.Coda attenuation Q-c1 of each station was firstly calculated by single scattering method. Then, mean free path Le and seismic albedo Bo of each station were calculated, and scattering attenuation Q-1s and intrinsic attenuation Q-1i were separated from total attenuation Q-1t by multiple lapse time window analysis based on the multiple scattering model in uniform random isotropic scattering medium. The attenuating characteristics in Yunnan show that most value of Le are in 10～30 km, with maximal within 2～6 Hz;Bo are about 0.5 at 1～2 Hz, but less than 0.5at other frequency-bands, which means Q-1i is comparable with Q-1s at 1～2 Hz, and after 1～2 Hz, Q-1i is greater than Q-1s and dominates the attenuation process. Q-1c is close to Q-1i at other frequency bands except 1～2 Hz.Results show that Q-1 especially Qs-1 varies spatially, Q-1 in eastern Yunnan zone is a bit higher than in northwestern Yunnan zone;northwestern Yunnan zone higher than southwestern Yunnan zone. Comparing with other results in global, Qs-1 in Yunnan is lower than the global average value among these results, Q-1i is higher than the global average value, and Q-1t lies the middle among these results.  相似文献   

Joint processing and analysis of seismic gravity measurements in Capital Circle area     

贾民育马丽  刘少明张晶孙少安  王武星 《地震学报(英文版)》2006,19(4):438-447

In Capital Circle area, there are three groups of repeated gravity measurements observed by different institutes using different instruments or methods. The simultaneous adjustment of absolute and relative measurements and the elimination of systematic error among the relative measurements have been carded out in this paper. Thus an unified temporal gravity change system with absolute reference has been established. On the basis of this, the crustal subsidence effect on gravity, which belongs to non-tectonic factor, is analyzed and the station displacement corrections are carried out, so that the long-wave disturbance is eliminated. So far our following aims are realized： the advantages of the absolute and relative measurement methods are complementary to each other; the contradiction and environment disturbance are eliminated; the amounts of information are enlarged; the sampling interval of time domain is compressed. In a word, the ability of identifying the tectonic activity process is enhanced. The results show that： there are systematic errors between the two groups of relative measurements and within the data of 10 campaigns ; the uneven local crustal subsidence in the southeast of the study area results in a linear rise of gravity value at 10 stations; they can be corrected by the regression analysis. The maps of revised temporal gravity change can obviously and integrally reflect the Ms=5.0 earthquake in Guye on October 6, 1995.  相似文献   

Multi-scale wavelet separation of aeromagnetic anomaly and study of faults in Beijing area     

张先 赵丽刘天佑  杨宇山 《地震学报(英文版)》2006,19(5):542-551

Introduction As the capital of China, Beijing is a major political, economic and cultural center. In 2008, it will host the Olympic Games. Therefore, Beijing is of great importance in our national undertak-ing in guarding against earthquakes and reducing their damages. The Chinese Capital Circle re-gion has always been attached great importance in monitoring earthquakes by the China Earth-quake Administration, and as the kernel of the Capital Circle region, Beijing is the key area for ea…  相似文献   

Study on NDVI- T _s space by combining LAI and evapotranspiration     

Han Lijuan  Wang Pengxin  Yang Hua  Liu Shaomin  Wang Jindi 《中国科学D辑(英文版)》2006,49(7):747-754

This paper focuses on interpreting the different spatial relationships between NDVI and T _s, a triangular or a trapezoid, and on analyzing transformation conditions, the physical and ecological meanings of the vegetation index-surface temperature space as well. Further, we use the Temperature-Vegetation Dryness Index (TVDI) to explain the existent meaning of a triangular space after NDVI reaches its saturated state by employing the relationships between NDVI, LAI and evapotranspiration. The specific relations between NDVI and T _s are useful for describing, validating and updating land surface models.  相似文献   

2005年10月巴基斯坦MW7.6地震对余震的触发研究   总被引：6，自引：0，他引：6  

万永革  沈正康  尚丹 《中国地震》2006,22(3):277-286

本文研究分析了2005年10月8日巴基斯坦主震产生的库仑破裂应力变化对余震的影响。计算时考虑了以下因素：（1）断层泥区域的孔隙流体压力和介质弹性常数与周围介质中的不同；（2）地震震源区的构造应力场方向；（3）将震源区构造应力和主震破裂产生的应力叠加计算得到余震破裂机制。该研究考虑了多种因素，计算结果与余震的分布比较吻合。结果表明2005年10月8日巴基斯坦主震对大部分余震有触发作用。  相似文献   

澜沧江大朝山水库蓄水前的地震活动本底     

李永莉  秦嘉政 《地震研究》2006,29(3):221-224

分析了大朝山水库蓄水前，水库区域历史中强、强地震背景与1992年来的地震活动格局，及蓄水前9年中库坝区天然地震活动的时、空、强分布，结果表明：大朝山水库区为地震活动水平较低的区域，库坝附近30km以2、3级地震活动为主，库首方向距大坝40km左右的景谷与库尾方向距大坝50km的昌宁、凤庆一带为5级地震活动区，外围100km左右的耿马、澜沧、普洱等地区为6、7级强震活动区；库坝区的地震活动基本符合G—R关系式，b值为0．69，累积应变曲线呈稳定增长趋势，时间分布上出现活跃与平静交替的分布格局。  相似文献   

华北地区未来50年地震危险性与强震预测研究     

张卫东  李茂林  王九洋  史宏伟 《东北地震研究》2006,22(4):6-13

本文对文献[1]、[2]的某些结论和结果作了认真的分析和讨论,提出了不同的观点。应用极值理论和b值方法对华北地震区未来50年的地震危险性和活动水平进行了分析,给出了各震级档次地震发生的概率预测。  相似文献   

华东地区测震学指标异常配套和中强震对应关系初探     

沈小七  陈宇卫 《东北地震研究》2006,22(4):25-29

本文分析了部分地震学指标的物理意义。通过对华东地区1970年以来14个指标的全时间扫描,并使用华东地区Ms≥5.0地震进行对应,结果表明,选取Rm值、b值和AC值进行同步异常分析,能显著提高华东地区的有震报震率,但有漏报。对目前华东地区异常集中区(南黄海及其沿岸地区)进行时间扫描,结果显示该异常集中区未出现同步异常,认为该区域短期内发生中强地震的可能性不大。  相似文献   

Carbon isotope ratios of C_4 plants in loess areas of North China     

WANG Guoan  HAN Jiamao  ZHOU Liping  XIONG Xiaogang  TAN Ming  WU Zhenhai  PENG Jun 《中国科学D辑(英文版)》2006,49(1)

Recent stable carbon isotope studies have shown that the occurrence of C4 plants on the Earth was much later than that of C3 plants and there was a global ex-pansion of C4 biomass around 5―8 million years ago[1]. Although far fewer species use the C4 pat…  相似文献