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1.
利用由149个台站记录的中国地震年报、四川和云南区域地震台网观测报告的5897个近震的27530条横波振幅与周期资料，反演得到川滇地区及周边的地壳衰减Q0值（频率为1 Hz时的Q值）空间分布图像、台站的场地响应以及由于介质衰减不同造成的震级偏差.结果表明，川滇及周边地区的地壳横波衰减Q0值在200～600范围内变化，平均值为400，横向变化显著.在川西-滇西北-保山地区、云贵交界-昆明-思茅地区以及海原-祁连、汾渭和东昆仑等活动块体边界带的Q0值明显较低，这些地区地震和构造活动相对活跃；而构造相对稳定的四川盆地、马尔康块体、桂西滇东断块以及鄂尔多斯、秦岭-大别等地区的Q0值则明显较高.此外，川滇地区大多数台站的场地响应都在1附近，仅有少数增益或衰减较大，达到2倍左右，且其分布无明显规律性.该区观测报告给出的大多数地震震级偏差不大于03，但也有少数震级偏差达04，其分布与介质品质因子Q0值分布相关，说明震级测定可能受地壳介质衰减横向变化的影响. 相似文献
2.
利用甘肃地震台网16个台站记录的远震资料，采用最大熵谱反褶积方法，得到了各个台站的接收函数. 采用接收函数扫描法和线性反演方法对研究区的壳幔结构进行了研究，这两种接收函数方法得出的结果具有很好的一致性. 青藏高原东北缘地壳厚度变化剧烈，祁连块体为50～55 km、柴达木块体和河西走廊为45 km左右（合作台除外），由北向南，Moho界面呈中央下凹的准对称状. 研究区地壳VP/VS介于166～185（σ=0215～0294，均值0254），其均值接近或略低于全球平均值；S波速度结构可见壳幔过渡带具有明显的突跳，结合其他地球物理学证据，推断该区可能不存在岩浆底侵作用和地壳部分熔融现象. 该区地壳VP/VS值与地壳厚度呈反相关关系，推断该区地壳的主要组成成分以中酸性岩石为主，其45～55 km厚的地壳可能主要是通过上地壳的叠置形成的. 相似文献
3.
利用震源距23 km范围内观测的2000年姚安MS65地震余震记录，计算了震源及近邻区域的尾波规一直达S波在频率15～20 Hz之间的傅里叶谱振幅.结果显示谱振幅随震源距增大而增大， 在对谱振幅进行了震源辐射方向性校正之后, 才出现谱振幅随震源距衰减的现象.由此获得了震源及近邻区域S波的Q(f)值,可表示为QS(f)=89f098其值比由尾波得出的姚安地区的平均QC(f)值低得多，表明了震源破裂带的强烈非均匀性对QS(f)的重大影响. 相似文献
4.
利用震源距23 km范围内观测的2000年姚安MS65地震余震记录，计算了震源及近邻区域的尾波规一直达S波在频率15～20 Hz之间的傅里叶谱振幅.结果显示谱振幅随震源距增大而增大， 在对谱振幅进行了震源辐射方向性校正之后, 才出现谱振幅随震源距衰减的现象.由此获得了震源及近邻区域S波的Q(f)值,可表示为QS(f)=89f098其值比由尾波得出的姚安地区的平均QC(f)值低得多，表明了震源破裂带的强烈非均匀性对QS(f)的重大影响. 相似文献
5.
选取云南地震台网记录的地震波形资料,通过基于遗传算法的Atkinson方法分别计算云南3个区域的介质品质因子Q_0值。根据云南地区地震波衰减的区域性差异,通过震级偏差统计分析了47个台站的单台M_L震级偏差情况。结果显示:云南属于低Q_0值地区,区域性差异明显。位于云南西部区域1的Q_0值相对较高,为251. 3;东部的区域3的Q_0值次之,为216. 9;中部的区域2的Q_0值最低,为102. 6。Q_0值越小的地区,S波衰减程度越大,单台震级偏小于台网平均震级的台站也就越多。同一地区的台站在测定相同区域内的地震时,虽然地震波非弹性衰减程度相近,但由于受到各台站场地不同增益作用的影响,其单台震级偏差情况有所不同。 相似文献
6.
《地震地质》2016,(4)
利用四川区域地震台网的数字波形资料以及中国地震台网中心的有关震相数据,选取互相衔接的3段地震波几何衰减模型,利用基于遗传算法的Atkinson和Mereu方法,分别反演四川盆地、川西高原及攀枝花—西昌地区的介质品质因子。采用Brune的ω平方模型约束震源位移谱,使用Moya方法联合多台多地震数据求得各地震台站的场地响应。根据波形数据和观测报告,计算出2009年1月1日至2015年6月30日10535次2.5≤M_L≤4.9近震单台震级测定值与台网平均震级的差,绘制各次地震的单台震级偏差空间分布图像。结果显示:四川盆地介质衰减模型呈现高Q_0和低衰减系数γ的特点,攀西地区表现出低Q_0和较高衰减系数γ;岩石台基对地震波信号在不同频率点的放大作用不相同;单台震级偏差优势分布基本一致,在构造稳定的四川盆地,介质品质因子高(低衰减),地震波在该区域能有效传播,盆地表层松软沉积层对入射波有放大作用,造成该区域单台震级高异常;川西大部分地震台站台基增益较大,但单台震级明显偏低,推测与松潘-甘孜块体地壳深度软流圈的物质流动及该区域低Q_0异常(高衰减)有关;攀西地区断陷拉张、流体侵入及沉积填充等损耗地震波能量,常使该地区台站测定的川西藏东地震震级偏小,但同样台站测定的龙门山断裂带上中强地震震级常较台网平均震级更大,可能是受盆地边缘强烈不对称高幅值带的影响。从研究结果看,四川地区介质衰减对地震射线振幅的影响较地震台站的台基增益大,因此校正四川区域地震台网单台震级时,应结合介质衰减及台站场地响应的空间特性进行考虑。 相似文献
7.
本文利用《中国地震年报》中测定震级ML时所用的区域地震图中水平向的最大振幅及周期资料，研究了地壳内横波的衰减及介质品质因子Q0特征. 结果表明，中国整个区域平均的Q0值为367，以华南地台最高，为460，塔里木盆地为442，鄂尔多斯高原为419，华北地区最低，为294，其次是川滇地区为295. 由这个结果可知，Q0与地质构造之间存在明显的相关特征，在构造上稳定的克拉通地台，如塔里木盆地、鄂尔多斯高原、华南地台等具有较高的Q0值；而构造上活动的强烈剪切变形带和新生代扩张盆地，如川滇地区和华北断陷盆地往往是Q0值低的地区，这和Pn速度分布特征也很相似，在Pn速度高的地区地壳Q0值亦高，在Pn速度低的地区Q0值亦低. 相似文献
8.
利用安芝的尾波公式,使用单台多震记录分别计算了各个台站周围地壳介质的平均Q值及台站和震中间地壳介质的Q值。结果表明,各地Q值均在100—300之间,只有少数地区超过300,和川滇交界区、昆明地区、宁夏地区相似,属于低Q值地区。定襄—代县、右玉—繁峙、定襄—原平、闻喜—绛县、闻喜—永济、太原—娄烦Q值在300以上;临汾—绛县、临汾—秸山、临汾—洪洞、太原附近次之,其Q值在240以上,其它地区Q值多在150左右。高Q值地区表明该区地壳介质强度大,地震波衰减慢,易于积累应变能。 相似文献
9.
烈度计台与测震台的布设环境、仪器类型不同，所测定的震级值存在一定差异。收集2017-2019年川滇地区301个烈度计台站记录的46次ML 3.0以上地震，进行震级校正。统计烈度计实测震级值与测震台网平均震级值的偏差，对原量规函数进行修正，进而做台站校正。综合修正后，利用量规函数和台站校正值重新计算烈度计震级，结果表明：在震中100 km范围内，烈度计测定震级偏差平均值由校正前的0.145降低至0.033，标准差由0.382降低至0.295，离散度减小；校正后的烈度计震级结果较优，说明本研究获得的量规函数和台站校正值更加适用于川滇地区烈度计台站的震级计算。 相似文献
10.
利用云南和四川数字地震观测台网记录的数字化地震资料,开展了川滇地区不同频率的QLg层析成像研究,反演结果的空间分辨率小于100 km.反演结果表明,川滇地区介质的横向不均匀性强烈,QLg高低值差异显著.川滇地区显著的高衰减区有川滇菱形块体的东南边界（即沿鲜水河至安宁河以及思茅—澜沧—普洱区）,滇西北地区、龙门山断裂以西松潘—茂文地区、巴塘及理塘强震区等,Lg波高衰减区的分布与构造活动强烈、强震活动或大震破裂造成介质破碎区、低速区等相关,表明构造活动强烈或大震破裂造成的介质破碎、热物质沿活动断裂上涌等可能是川滇地区低QLg的主要成因.显著的低衰减区有川东盆地、滇东南地区以及金沙江、怒江断裂的中段区域,滇中块体内部也呈现出相对的低衰减特征.Lg波低衰减区与地震活动性弱、速度正异常等相关,表明川滇地区Lg波的低衰减区与地壳变形、地震活动性及水热活动弱、块体稳定等有关. 相似文献
11.
Structure and Significance of S-wave Velocity and Poisson’s Ratio in the Crust beneath the Eastern Side of the Qinghai-Tibet Plateau 总被引：2，自引：0，他引：2
The receiver functions of body waves of distant earthquakes obtained for the regions beneath 41 digital stations (Lhasa and
GANZ in Tibet, Mandalay and Rangoon in Myanmar, SHIO in India, CHTO in Thailand, and station network in Sichuan and Yunnan)
were used to invert for S-wave structure in the crust and upper mantle in Sichuan, Yunnan, and their surrounding areas. Meanwhile
the distribution characteristics of the Poisson’s ration and the crustal thickness in Sichuan and Yunnan areas were also obtained.
Results indicate that the depth of Moho beneath the eastern side of Qinghai-Tibetan plateau varies strikingly. It is obvious
that the greatest changes in crustal thickness occur in a north-south direction. The crustal thickness decreases from north
to south, being as thick as 70 km in eastern Tibet, the northern portion of our area of interest, and less than 30 km in Chaing
Mai and Rangoon, the southern portion of our area. There are, however, exceptions regarding the trend. The thickness exhibits
an east-west variation trend in the area from Ma’erkong-Kongding in Sichuan to Lijiang in Yunnan. In general the Jinpingshan-Longmenshan
fault and Anninghe fault can be taken as the boundaries of this exception area. The thickness in Kongding in the west is 68 km,
while it is only 39 km in Yongchuan in the east. Moreover the Poisson’s ratio values in the blocks of central Sichuan and
Sichuan-Yunnan Diamond are high, and a low velocity layer in the crust of this area can be obviously detected. The distribution
characteristics of the high Poisson’s ratio and the low velocity of the crust in this block correspond to the tectonic structure,
being in contrast with the surrounding areas. Combining with the distribution features of the modern tectonic stress field,
it is deduced that the Sichuan-Yunnan area is probably the channel through which the materials of the lithosphere flow eastward. 相似文献
12.
Fine structure of Pn velocity beneath Sichuan-Yunnan region 总被引：3，自引：0，他引：3
We use 23298 Pn arrival-time data from Chinese national and provincial earthquake bulletins to invert fine structure of Pn velocity and anisotropy at the top of the mantle beneath the Sichuan-Yunnan and its adjacent region. The results suggest that the Pn velocity in this region shows significant lateral variation; the Pn velocity varies from 7.7 to 8.3 km/s. The Pn-velocity variation correlates well with the tectonic activity and heat flow of the region. Low Pn velocity is observed in southwest Yunnan , Tengchong volcano area, and the Panxi tectonic area. These areas have very active seismicity and tectonic activity with high surface heat flow. On the other hand, high Pn velocity is observed in some stable regions, such as the central region of the Yangtze Platform; the most pronounced high velocity area is located in the Sichuan Basin, south of Chengdu. Pn anisotropy shows a complex pattern of regional deformation. The Pn fast direction shows a prominent clockwise rotation pattern from east of the Tibetan block to the Sichuan-Yunnan diamond block to southwest Yunnan, which may be related to southeastward escape of the Tibetan Plateau material due to the collision of the Indian Plate to the Eurasia Plate. Thus there appears to be strong correlation between the crustal deformation and the upper mantle structure in the region. The delay times of events and stations show that the crust thickness decreases from the Tibetan Plateau to eastern China, which is consistent with the results from deep seismic sounding. 相似文献
13.
We use 23298 Pn arrival-time data from Chinese national and provincial earthquake bulletins to invert fine structure of Pn velocity and anisotropy at the top of the mantle beneath the Sichuan-Yunnan and its adjacent region. The results suggest that the Pn velocity in this region shows significant lateral variation; the Pn velocity varies from 7.7 to 8.3 km/s. The Pn-velocity variation correlates well with the tectonic activity and heat flow of the region. Low Pn velocity is observed in southwest Yunnan, Tengchong volcano area, and the Panxi tectonic area. These areas have very active seismicity and tectonic activity with high surface heat flow. On the other hand, high Pn velocity is observed in some stable regions, such as the central region of the Yangtze Platform; the most pronounced high velocity area is located in the Sichuan Basin, south of Chengdu. Pn anisotropy shows a complex pattern of regional deformation. The Pn fast direction shows a prominent clockwise rotation pattern from east of the Tibetan block to the Sichuan-Yunnan diamond block to southwest Yunnan, which may be related to southeastward escape of the Tibetan Plateau material due to the collision of the Indian Plate to the Eurasia Plate. Thus there appears to be strong correlation between the crustal deformation and the upper mantle structure in the region. The delay times of events and stations show that the crust thickness decreases from the Tibetan Plateau to eastern China, which is consistent with the results from deep seismic sounding. 相似文献
14.
QI Yu-ping ZHANG Zhi-wei LONG Feng XIAO Ben-fu LIANG Ming-jian LU Qian JIANG Peng 《地震地质》2018,40(2):377-395
The Daliangshan sub-block is a boundary region among the Bayan Har block, the Sichuan-Yunnan block and the South China block. It hosts four major fault systems:The southwest to south trending Xianshuihe-Zemuhe Fault zone in the west, the Longmenshan fault zone is the northern boundary, the Zhaotong-Lianfeng fault zone in the south, and the NS-trending Mabian-Yanjin fault zone in the east. This study focused on focal mechanisms and the regional stress field of the Daliangshan sub-block to help understand the earthquake preparation process, tectonic deformation and seismic stress interaction in this area. We collected broadband waveform records from the Sichuan Seismic Network and used multiple 1-D velocity models to determine the focal mechanisms of moderate and large earthquakes(ML ≥ 3.5)in the Daliangshan sub-block by using the CAP method. Results for 276 earthquakes from Jan 2010 to Aug 2016 show that the earthquakes are dominated by strike-slip and trust faulting, very few events have normal faulting and the mixed type. We then derived the regional distribution of the stress field through a damp linear inversion(DRSSI)using the focal mechanisms obtained in this study. Inversion results for the spatial pattern of the stress field in the block suggest that the entire region is predominantly under strike-slip and trust faulting regimes, largely consistent with the focal mechanisms. The direction of maximum compression axes is NW-NWW, and part of the area is slightly rotated, which is consistent with the GPS velocity field. Combining geodynamic background, this work suggests that because the Sichuan-Yunnan block is moving to SE and the Tibetan plateau to SE-E along major strike-slip faults, the stress field of the Daliangshan sub-block and its adjacent regions is controlled jointly by the Bayan Har block, the Sichuan-Yunnan block and the South China block. 相似文献
15.
利用云鹏水电站周边5个数字地震台站记录到的2000年1月至2008年12月间的108个地震的数字波形资料,采用Aki单次散射模型,计算了各台站周围423条地震记录的尾波Q0值。结果显示:云鹏水电站地区尾波的Qc值与频率的关系为Qc(f)=90.2f0.94。该地区的Q0值比云南其它构造活动强烈地区的要高,因此属于中等构造活动地区。云鹏水电站蓄水后弥勒台记录到的108个地震的尾波Q0值及分频Qc值有所下降,但下降幅度不大,表明水库蓄水对库区及其附近区域地下介质性质有所影响,但影响的程度有限。 相似文献
16.
川滇地区中小震重新定位与速度结构的联合反演研究 总被引：8，自引：0，他引：8
通过震源与速度结构联合反演, 利用2000年4月至2006年3月云南和四川区域地震台网给出的P波初至走时资料, 确定了川滇地区的三维速度结构, 同时获得了川滇地区6642次中小地震的重新定位结果。 结果表明: ① 川滇地区地震震源平均深度随震级增大而加深的特征明显, 地震震级越大, 震源深度越深, 但震源下界不超过25 km; ② 在瑞丽-龙陵、 丽江-小金河以及龙门山等断裂带以西地区, 震源深度偏浅, 大多在15 km以上, 15 km深度以下地震稀少; ③ 川滇地区中小地震分布具有与强震相同的地壳深部介质背景, 震源大多分布于正、 负异常过渡区的速度相对较高一侧, 而其下方主要为低速异常分布。 相似文献
17.
18.
The Shimian area of Sichuan sits at the junction of the Bayan Har block, Sichuan-Yunnan rhombic block, and Yangtze block, where several faults intersect. This region features intense tectonic activity and frequent earthquakes. In this study, we used local seismic waveform data recorded using dense arrays deployed in the Shimian area to obtain the shear wave splitting parameters at 55 seismic stations and thereby determine the crustal anisotropic characteristics of the region. We then analyzed the crustal stress pattern and tectonic setting and explored their relationship in the study area. Although some stations returned a polarization direction of NNW-SSE, a dominant polarization direction of NW-SE was obtained for the fast shear wave at most seismic stations in the study area. The polarization directions of the fast shear wave were highly consistent throughout the study area. This orientation was in accordance with the direction of the regional principal compressive stress and parallel to the trend of the Xianshuihe and Daliangshan faults. The distribution of crustal anisotropy in this area was affected by the regional tectonic stress field and the fault structures. The mean delay time between fast and slow shear waves was 3.83 ms/km, slightly greater than the values obtained in other regions of Sichuan. This indicates that the crustal media in our study area had a high anisotropic strength and also reveals the influence of tectonic complexity resulting from the intersection of multiple faults on the strength of seismic anisotropy. 相似文献