The 1998 Hida Mountain, Central Honshu, Japan, earthquake swarm: Double-difference event relocation, frequency–magnitude distribution and Coulomb stress changes     

Bogdan Enescu  Kiyoshi Ito   《Tectonophysics》2005,409(1-4):147-157

By using the double-difference relocation technique, we have determined the fine structure of seismicity during the 1998 Hida Mountain earthquake swarm. The distribution of seismic activity defines two main directions (N–S and E–W) that probably correspond to the regional stress pattern. The detailed structure of seismicity reveals intense spatio-temporal clustering and earthquake lineations. Each cluster of events contains a mainshock and subsequent aftershock activity that decays according to the Omori law. The seismicity and the b-value temporal and spatial patterns reflect the evolution of the static stress changes during the earthquake swarm. About 80% of the swarm's best-relocated events occur in regions of increased ΔCFF. The smaller value of b found in the northern part of the swarm region and a larger b-value observed to the south, for the same period of time, could be well explained by the static stress changes caused by the larger events of the sequence. We argue that the state of stress in the crust is the main factor that controls the variation of b-value.  相似文献   

Relocation and assessment of seismicity in the Iran region   总被引：11，自引：0，他引：11  

E. Robert Engdahl  James A. Jackson  Stephen C. Myers  Eric A. Bergman  Keith Priestley 《Geophysical Journal International》2006,167(2):761-778

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High-precision relocation and focal mechanism of the 2002 rain-triggered earthquake swarms at Mt Hochstaufen, SE Germany   总被引：1，自引：0，他引：1  

T. Kraft  J. Wassermann  H. Igel 《Geophysical Journal International》2006,167(3):1513-1528

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2003年青海德令哈地震序列的重新定位和发震构造   总被引：4，自引：0，他引：4  

孙长虹  钱荣毅  肖国林  孟小红 《物探与化探》2006,30(1):79-82

应用交切法对2003年4月17日德令哈地震序列的M_L=6.7主震和截止至2003年10月25日的M_L小于1.0级的余震,共117次地震事件进行了初始定位,并以双差地震定位法对这些地震重新进行精确定位。认为德令哈地震序列的主震震中位置为37.566°N,96.509°E,震源深度为13km,余震震源空间位置分布与哈佛大学震源机制解给出的走向为294°的节面一致。德令哈地震序列重新精确定位的结果清楚地表明了穿过震区的走向NWW—SEE、倾向NE的大柴旦—宗务隆山现代活动断裂带是这次德令哈地震序列的发震构造,同时表明该区域应力场水平最大主应力方向范围大致在N24°E—N34°E。  相似文献   

中性和不稳定层结大气的孤立行波精确解     

周江兴  丁一汇  刘益民 《气象学报》1996,54(2):195-206

通过研究二维准动量无辐散、无摩擦层结大气非线性方程组的行波解问题证明，非线性行波解的本质属性是由参数ｂ的符号性质决定的。当ｂ＞０时，为周期解，其周期与相应的线性周期解的周期相等；当ｂ≤０时，为孤立波解。给出了一般行波解的解析表达式。并细致地研究了中性和不稳定层结大气中的孤立行波的特征，发现中性和不稳定层结大气中存在具有类似于飑线结构特征的孤立波。指出了中性和不稳定层结大气中的一般孤立行波物理量的分布特征。  相似文献   

Relocation and seismogenic structure of the 1998 Zhangbei-Shangyi earthquake sequence     

杨智娴  陈运泰  张宏志 《地震学报(英文版)》2002,15(4):383-394

Introduction The January 10, 1998 Zhangbei-Shangyi, Hebei Province, earthquake has been the third large event of magnitude 6.0 and greater since the 1976 great Tangshan earthquake of magnitude 7.8 in the northern China (33皛42癗, 110皛124癊). Before this event, there were only two events of magnitude 6.0 and greater occurred in or around the Tangshan area since 1976: the M=6.9 Ninghe, Tianjin, earthquake of November 15, 1976 and the M=6.2 Hangu, Tianjin, earthquake of May 12, 1977. The …  相似文献   

Relocation of the Ms≥2.0 Earthquakes in the Northern Tianshan Region, Xinjiang, Using the Double-Difference Earthquake Relocation Algorithm     

Wang Haitao 《中国地震研究》2007,21(4):388-396

We applied the double-difference earthquake relocation algorithm to 1348 earthquakes with M_S≥2.0 that occurred in the northern Tianshan region, Xinjiang, from April 1988 to June 2003, using a total of 28701 P- and S-wave arrival times recorded by 32 seismic stations in Xinjiang. Aiming to obtain most of these M_S≥2.0 earthquakes relocations, and considering the requirements of the DD method and the condition of data, we added the travel time data of another 437 earthquakes with 1.5≤M_S<2.0. Finally, we obtained the relocation results for 1253 earthquakes with M_S≥2.0, which account for 93% of all the 1348 earthquakes with M_S≥2.0 and includes all the M_S≥3.0 earthquakes. The reason for not relocating the 95 earthquakes with 2.0≤M_S<3.0 is analyzed in the paper. After relocation, the RMS residual decreased from 0.83s to 0.14s, the average error is 0.993 km in E-W direction, 1.10 km in N-S direction, and 1.33 km in vertical direction. The hypocenter depths are more convergent than before and distributed from 5 km to 35 km, with 94% being from 5km to 35 km, 68.2% from 10 km to 25 km. The average hypocenter depth is 19 km.  相似文献   

The 9th of July 1998 Faial Island (Azores,North Atlantic) seismic sequence   总被引：2，自引：0，他引：2  

L. Matias  N. A. Dias  I. Morais  D. Vales  F. Carrilho  J. Madeira  J. L. Gaspar  L. Senos  A. B. Silveira 《Journal of Seismology》2007,11(3):275-298

The Faial earthquake (M _L 5.8) that occurred on the 9th of July, 1998, in the Azores region (north Atlantic), caused nine casualties and severe destruction affecting more than 5,000 people. The main shock was located at sea, 10 km NE of the Faial Island, and triggered a seismic sequence that lasted for several weeks and was characterized by an unusual high p-value of 1.40 for the modified Omori law. We present here the results of a joint inversion of hypocenters and 1D velocity model performed on the data collected by the permanent network complemented with a temporary network installed shortly after the occurrence of the main event. The 1D velocity model shows a heterogeneous upper crust, testified by the observed differences in site effects at the stations, while the middle crust from ∼2.5 to 8 km in depth is quite homogeneous. The Moho is located at a depth of about 12–13 km and the Vp/Vs ratio is found to be around 1.78. The events at depth are mainly concentrated in the middle-lower crust (8–12 km), while their spatial distribution shows a main cluster, visible after relocation, SSE trending. This direction of elongation is consistent with one of the fault planes (N151°E) of the centroid moment tensor (CMT) solution for the main shock. The same plane is the preferred main shock fault plane inferred after a Coulomb failure function analysis on the aftershock distribution. The main event relocation points to a focal depth shallower than 5 km. The aftershocks pattern shows that several fault systems were reactivated by the stress perturbation induced by the main shock. Besides the two main tectonic directions, trending WNW–ESE and NNW–SSE, observed in the tectonics of Faial, Pico, and S. Jorge, there is also evidence of a new tectonic direction trending WSW–ENE.  相似文献   

生命周期视角下建成环境对居民迁居强度的影响——基于武汉市多源数据分析     

刘华  周田原  张贵科  刘学军  邓韶辉 《地理科学进展》2023,42(1):66-78

随着中国城镇住房制度改革的推行,城市内迁居行为日趋频繁。洞悉不同年龄段居民迁居内在驱动力,能为城市居住环境规划与建设改善提供依据。论文利用2019年与2021年武汉市手机信令等多源数据,以生命周期理论为研究视角,识别武汉市四环内不同年龄段居民交通小区迁居强度,并提出建成环境因子特性与迁居强度关系模型,探讨居民生活圈内各建成环境因子对多年龄段居民迁居影响的特性差异。研究发现：(1)不同年龄居民的迁入与迁出强度在不同城市区位上存在分异,19～39岁居民相较于40岁以上居民迁居更频繁;总体呈现内环线的交通小区迁入与迁出强度表征偏高,且均大于外环线的交通小区。(2)公共服务设施、交通便利度和居住环境维度内相关指标是影响居民迁居决策的重要因素,由于不同年龄段居民居住需求不同,部分变量因子在不同年龄段下特性分异明显。考虑到各年龄段居民迁居强度及因子特性不一,相关规划决策需采取差异化的建成环境改善措施,科学引导不同年龄居民迁居,优化城市人口分布。  相似文献   

Wildfire-Migration Dynamics: Lessons from Colorado's Fourmile Canyon Fire     

Raphael J. Nawrotzki  Hannah Brenkert-Smith  Lori M. Hunter  Patricia A. Champ 《社会与自然资源》2014,27(2):215-225

The number of people living in wildfire-prone wildland–urban interface (WUI) communities is on the rise. However, no prior study has investigated wildfire-induced residential relocation from WUI areas after a major fire event. To provide insight into the association between sociodemographic and sociopsychological characteristics and wildfire-related intention to move, we use data from a survey of WUI residents in Boulder and Larimer counties, Colorado. The data were collected 2 months after the devastating Fourmile Canyon fire destroyed 169 homes and burned more than 6,000 acres of public and private land. Although this study is working with a small migrant sample, logistic regression models demonstrate that survey respondents intending to move in relation to wildfire incidence do not differ sociodemographically from their nonmigrant counterparts. They do, however, show significantly higher levels of risk perception. Investigating destination choices shows a preference for short-distance moves.  相似文献