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Earthquake relocation and 3-dimensional crustal structure of P-wave velocity in cen-tral-western China 被引量:26
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作者 杨智娴 于湘伟 +3 位作者 郑月军 陈运泰 倪晓晞 Winston CHAN 《地震学报》 CSCD 北大核心 2004年第1期19-29,共11页
采用中国中西部地区(2l°~36°N,98°~112°E)193个地震台在1992~1999年间记录到的9988次地震的Pg和Sg震相走时的读数资料,用Roecker的SPHYPIT90程序,反演了该地区三维地壳P波速度结构,并用SPHREL3D90程序进行... 采用中国中西部地区(2l°~36°N,98°~112°E)193个地震台在1992~1999年间记录到的9988次地震的Pg和Sg震相走时的读数资料,用Roecker的SPHYPIT90程序,反演了该地区三维地壳P波速度结构,并用SPHREL3D90程序进行了地震的重新定位.反演结果揭示了中国中西部地区地震P波速度结构明显的横向不均匀性,这些不同深度上波速的横向变化多以该地区的活动断裂为分界线.可以看出活动断裂两侧存在明显的速度反差.通过重新定位,得到了6459次地震的震源参数,这些精确定位的地震震中明显沿该区活动断裂呈现条带状分布,其范围和尺度清晰地表示了这一地区地震活动与活动断裂的紧密关系.其中,82%重新精确定位的事件的震源深度在20km以内.这一结果与笔者用双差地震定位法得到的重新定位的震源深度分布相一致. 展开更多
关键词 地震重新定位 P波速度结构 反演 双差地震定位法 地震活动 活动断裂
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Discussion on origin of Pn velocity variationin China and adjacent region 被引量:14
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作者 裴顺平 许忠淮 汪素云 《地震学报》 CSCD 北大核心 2004年第1期1-10,共10页
Pn velocity lateral variation and anisotropy images were reconstructed by adding about 50 000 travel times from the regional seismic networks to the datum set of near 40 000 travel times from National Seismic Network ... Pn velocity lateral variation and anisotropy images were reconstructed by adding about 50 000 travel times from the regional seismic networks to the datum set of near 40 000 travel times from National Seismic Network of China used by WANG, et al. We discussed the relation of Pn velocity variation to Moho depth, Earths heat flow, distribution of Cenozoic volcanic rock and the result of rock experiment under high pressure and high temperature. The result of quantitative analysis indicates that Pn velocity is positively correlated with the crust thickness and negatively correlated with the Earths heat flow. Two linear regression equations, one between Pn velocity and crust thickness, and the other between Pn velocity and heat flow, were obtained. The rate of variation of Pn veloc-ity vP with pressure P, Pv/p, estimated from the velocity variation with crust thickness Hv/p, is close to the result obtained from the rock experiment under high pressure and high temperature. If the effect of crust thick-ness on Pn velocity is deducted from the velocity variation, then the low Pn velocity beneath Qinghai-Xizang pla-teau is more notable. The low Pn velocity regions well agree with the Cenozoic volcanic rock. In the several re-gions with significant anisotropy, the direction of fast Pn velocity is consistent with the orientation of maximum principal crustal compressive stress, and also with the direction of present-day crustal movement. It indicates that the fast Pn velocity direction may be related to the deformation or flow of top mantle material along the direction of maximum pressure. 展开更多
关键词 地震台网 PN波 地壳厚度 新生代 火山岩 各向异性 层析成像
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Strong earthquake activity all over the world and strong-moderate earthquake ac-tivity within and near China (April, 2004 ~ May, 2004)
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作者 陈培善 《地震学报》 CSCD 北大核心 2004年第5期565-566,共2页
关键词 地震参数 面波震级 地震仪 地理坐标
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The coda attenuation of the Yao'an area in Yunnan Province 被引量:61
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作者 李白基 秦嘉政 +1 位作者 钱晓东 叶建庆 《地震学报》 CSCD 北大核心 2004年第1期47-52,共6页
2000年1月15日云南姚安发生了6.5级地震.震后围绕震中区架设了一个由6套拾震器-记录仪组成的临时数字地震台网.在所记录的余震中,有402次余震有较精确的定位.依照Sato的单散射模型分析观测的尾波短记录,获得了姚安地区地壳的尾波... 2000年1月15日云南姚安发生了6.5级地震.震后围绕震中区架设了一个由6套拾震器-记录仪组成的临时数字地震台网.在所记录的余震中,有402次余震有较精确的定位.依照Sato的单散射模型分析观测的尾波短记录,获得了姚安地区地壳的尾波平均品质因子Qc(f)=49f^0.95,f=1.5~20.0Hz,具有高构造活动性区域的衰减特征. 展开更多
关键词 Sato单散射模型 尾波衰减 地震定位 地震波 数字地震台网
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Crustal structure in northern margin of Tianshan mountains and seismotectonics of the 1906 Manas earthquake 被引量:38
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作者 王椿镛 楼海 +1 位作者 魏修成 吴庆举 《地震学报》 CSCD 北大核心 2001年第5期460-470,共11页
长86 km、南北向横跨乌鲁木齐坳陷的深地震反射剖面,揭示了北天山山前地壳的薄皮构造特征.共深度点叠加剖面的石河子以南部分显示了天山北缘平行山体的第一和第二排背斜构造.与双程时间分别为2.5~3.0s和5.5~6.0s的反射事件对应的滑脱... 长86 km、南北向横跨乌鲁木齐坳陷的深地震反射剖面,揭示了北天山山前地壳的薄皮构造特征.共深度点叠加剖面的石河子以南部分显示了天山北缘平行山体的第一和第二排背斜构造.与双程时间分别为2.5~3.0s和5.5~6.0s的反射事件对应的滑脱构造,将地壳深部构造与地表逆断裂-褶皱构造联系在一起.玛纳斯断裂以铲形方式向下延伸,在2.5s左右深度归并于第一滑脱面,向南与清水河断裂汇合.在5.5~6.0s深度上为与玛纳斯下背斜相连的主滑脱面.它们最终汇集到准噶尔南缘断裂.石河子以北的坳陷沉积深度达12~14km.沿剖面的莫霍界面深度在准噶尔盆地为45km左右,往南加深至50km.对该区域内的深地震测深剖面和布格重力异常资料的分析结果,与深反射剖面的地壳结构图象具有一致性.深地震反射剖面通过1906年玛纳斯7.7级地震宏观震中区,共深度点叠加剖面用于推断玛纳斯7.7级地震与北天山山前地壳构造之间的关系:玛纳斯地震属于一类“褶皱地震”,其发震构造是由准噶尔南缘断裂、清水河逆冲断裂、滑脱面和玛纳斯浅部断坡组成的断层系. 展开更多
关键词 地壳结构 深地震反射剖面 逆断层-褶皱带 玛纳斯地震区 地震构造
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Quantitative data about active tectonics and possible locations of strong earthquakes in the future in the northwestern Beijing 被引量:20
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作者 冉勇康 陈立春 徐锡伟 《地震学报》 CSCD 北大核心 2001年第5期502-513,共12页
Deterministic, probabilistic and composite-grading methods are used to get the possible locations of strong earth-quakes in the future in Norwest Beijing and its vicinity based on the quantitative data and their accur... Deterministic, probabilistic and composite-grading methods are used to get the possible locations of strong earth-quakes in the future in Norwest Beijing and its vicinity based on the quantitative data and their accuracy about active tectonics in the research area and by ordering, some questions in the results are also discussed. It shows that the most dangerous fault segments for strong earthquakes in the future include: segments B and A of the southern boundary fault of the Yangyuan basin, the southern boundary fault of the Xuanhua basin, the east segment of the southern Huaian fault and the east segment of the northern YanggaoTianzhen fault. The most dangerous area is YangyuanShenjing basin, the second one is TianzhenHuaianXuanhua basin and the third dangerous areas are WanquanZhangjiakou and northeast of Yuxian to southwest of Fanshan. 展开更多
关键词 北京 活动构造定量资料 综合方法 强震地点 确定性方法 概率方法
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The algorithm of decomposing superim-posed 2-D Poisson processes and its applica-tion to the extracting earthquake clustering pattern 被引量:8
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作者 裴韬 周成虎 +2 位作者 杨明 骆剑承 李全林 《地震学报》 CSCD 北大核心 2004年第1期53-61,共9页
Aiming at the complexity of seismic gestation mechanism and spatial distribution, we hypothesize that the seismic data are composed of background earthquakes and anomaly earthquakes in a certain temporal-spatial scope... Aiming at the complexity of seismic gestation mechanism and spatial distribution, we hypothesize that the seismic data are composed of background earthquakes and anomaly earthquakes in a certain temporal-spatial scope. Also the background earthquakes and anomaly earthquakes both satisfy the 2-D Poisson process of different parameters respectively. In the paper, the concept of N-th order distance is introduced in order to transform 2-D superimposed Poisson process into 1-D mixture density function. On the basis of choosing the distance, mixture density function is decomposed to recognize the anomaly earthquakes through genetic algorithm. Combined with the temporal scanning of C value, the algorithm is applied to the recognition on spatial pattern of foreshock anomalies by exam-ples of Songpan and Longling sequences in the southwest of China. 展开更多
关键词 丛集地震 背景地震 混合泊松过程 遗传算法 混合密度分解
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Research on the effect estimation of seismic safety evaluation
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作者 邹其嘉 陶裕禄 《地震学报》 CSCD 北大核心 2004年第1期84-93,共10页
Seismic safety evaluation is a basic work for determining the seismic resistance requirements of major construc-tion projects. The effect, especially the economic effect of the seismic safety evaluation has been gener... Seismic safety evaluation is a basic work for determining the seismic resistance requirements of major construc-tion projects. The effect, especially the economic effect of the seismic safety evaluation has been generally con-cerned. The paper gives a model for estimating the effect of seismic safety evaluation and calculates roughly the economic effect of seismic safety evaluation with some examples. 展开更多
关键词 地震安全性评价 经济效益 社会效益 评估模型
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岩石变形破坏局部化的白光数字散斑相关方法研究(英文) 被引量:17
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作者 潘一山 杨小彬 马少鹏 《岩土工程学报》 EI CAS CSCD 北大核心 2002年第1期98-100,共3页
介绍了白光数字散斑法的基本原理 ,并采用白光数字散斑相关方法研究了煤岩的变形局部化 ,通过实验测定了煤岩变形局部化的开始时刻、演化过程 ,首次获得了局部化带的宽度 ,为研究岩石非均匀变形的演化过程。
关键词 岩石 变形局部化 白光数字散斑相关方法
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International Handbook of Earthquake and Engineer-ing Seismology 被引量:1
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作者 陈运泰 吴忠良 《地震学报》 CSCD 北大核心 2004年第1期110-111,共2页
关键词 国际地震学 工程地震学 《国际地震学与工程地震学手册》 国际地震工程协会
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Near Earth Vortices Driving of Field Aligned Currents Based on Magnetosphere Multiscale and Swarm Observations 被引量:1
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作者 ZHANG C SHEN C +8 位作者 YANG Y Y DUNLOP M W TI S RUSSELL C T LüHR H BURCH J L LINDQVIST P A TORBERT R B FRIIS-CHRISTENSEN E 《空间科学学报》 CAS CSCD 北大核心 2019年第1期9-17,共9页
A long-standing mystery in the study of Field-Aligned Currents(FACs) has been that: how the currents are generated and why they appear to be much stronger at high altitudes than in the ionosphere. Here we present two ... A long-standing mystery in the study of Field-Aligned Currents(FACs) has been that: how the currents are generated and why they appear to be much stronger at high altitudes than in the ionosphere. Here we present two events of magnetotail FACs observed by the Magnetospheric Multiscale Spacecraft(MMS) on 1 st July and 14 th July 2016, to show how the Substorm Current Wedges(SCW) were formed. The results show that particles were transferred heading towards the Earth during the expansion phase of substorms.The azimuthal flow formed clockwise(counter-clockwise) vortex-like motion, and then generated downward(upward) FACs on the tailward/poleward side of the distorted field with opposite vorticity on their Earthward/equatorward side. We also analyzed the Region 1 FACs observed by the Earth Explorer Swarm spacecraft on 1 st July 2016 and found that they were associated with FACs observed by MMS, although differing by a factor of 10. This difference suggests that either there was the closure of the currents at altitudes above 500 km or the currents were not strictly parallel to B and closed at longitudes away from where they were generated. 展开更多
关键词 SUBSTORM current WEDGE MAGNETOSPHERE Field-aligned CURRENTS Flow VORTICITY Multiple spacecraft measurements
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