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根据实地调查初步认为,1995年11月12日广东丰顺ML4.7级地震以震级较低但破坏显著,具有双极震区;震源深度大;宏观影响场分布与东西向为裂关系密切为其特征。地震发生在东西向和北东向并推断有北西向断裂穿越的地区。五华-丰良东西向断理解及河源=丰顺东西中断裂的东段是这次地震的主要发震断层。 相似文献
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用航磁资料研究了青海柴达木盆地中部的深部构造环境。结果表明:该地区存在由东西向、北西向和北东向各两条断裂组成的构造系统;地震主要分布在由两条东西向断裂和两条北东向断裂交截形成的顺扭平形四边形的角区;构造应力场主压应力方向大致为近南北方向,在其作用下,北东向和东西向断裂都是该地区主要的发震构造。 相似文献
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潮汕平原北西向断裂左旋走滑运动的地貌证据和速率 总被引:8,自引:0,他引:8
地处粤东的潮汕平原发育北西向与北东向两组活动断裂.经航片仔细解译,发现黄岗水断裂和丰顺-汕头断裂的部分段落呈明显水系左旋位错现象.野外调查证实了沿该两条断裂的地貌体位移,并选择3处位移点作了大比例尺地形图测绘,对被位移地貌体进行了采样测年.经计算,黄岗水断裂和丰顺-汕头断裂的全新世左旋走滑运动平均速率分别达1.11±0.09~2.69±0.24 mm/a和3.26±0.26 mm/a.这些较强活动的北西向断裂延伸入海与海域水深40~50m处的北东向牛山岛-兄弟屿-南澎列岛强活动断裂的交汇处是发生强震的有利部位. 相似文献
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福建沿海地区断裂构造发育,有北北东—北东向,北西向、东西向、南北向及环状或弧形断裂等构造系。近期以北北东—北东向压扭性断裂和北西向张扭性断裂活动性最强。它们控制着本区海岸地貌的发育以及地震的发生和分布。本文拟根据地壳垂直形变及海平面变化的资料,讨论本区有强震产生的活动断裂与地震活动。 相似文献
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东南沿海地区的断裂与地震 总被引:1,自引:0,他引:1
中国东部,相对来说东南沿海地区的地震活动较为频繁,断裂构造也十分发育。地震活动与断裂构造有非常密切的关系,震中与断裂构造的空间分布也关系密切。通过对东南沿海大量震例的调查和研究,分析三组断裂与地震的关系,得出东南沿海地区东西向、北东向和北西向的三组断裂构造,分别构成了区内的衰减构造、控震构造和发震构造,形成了东南沿海陆缘构造活动带。 相似文献
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We select the Xiluodu-Wudongde reservoir area in the downstream of Jinsha River as the research area, and use the CAP and GPAT method to obtain focal mechanisms of ML ≥ 2.0 earthquakes from 2016 to 2017 in this region. Then, we analyze the spatial distribution characteristics of focal mechanism solutions in each local region and investigate the relationship between seismicity and regional structures. According to 414 focal mechanism solutions we get following conclusions:1)The Xiluodu dam began to impound water on May 4, 2013, and seismicity increased significantly after impoundment. We get 49 focal mechanisms in the Xiluodu dam and its adjacent area which are dominated by thrust faulting and next by strike-slip faulting, which are mainly distributed near the middle section of the Ebian-Jinyang fault zone. The distribution of nodal planes striking in NNW to NE direction is consistent with that of regional faults, and some large earthquakes are controlled by regional structures. 2)There are 39 and 24 focal mechanisms obtained in the unimpounded Baihetan and Wudongde dams and adjacent areas, and the spatial distribution of focal mechanism solutions are relatively consistent, dominated by strike-slip faulting with a small amount of thrust and normal faulting. The sinistral strike-slip earthquakes are consistent with the activity of Xiaojiang fault zone and Puduhe-Xishan Fault. The strikes of the nodal planes are distributed discretely, and many groups of faults intersect with each other in the area, suggesting that the seismogenic environment is relatively complex. 3)The seismicity in Ludian continues to be active after the Ludian M6.5 earthquake. By the end of 2017, we got 260 focal mechanism solutions in the aftershock area of the Ludian MS6.5 earthquake of Aug 3rd, 2014, which show an "L-shape" in distribution and are dominated by thrust and strike-slip faulting. The long axis is distributed in EW direction, and the short axis is distributed in near NNW direction. The strikes of nodal planes are mainly near EW and near NE, and the nodal planes in the NW direction are less. According to characteristics of a large number of focal mechanism solutions, we deduce that there may exist a buried structure in the EW direction, the seismicity is controlled by different types of faults and the seismogenic structure is very complex. 4)The centroid depth in each region is concentrated in the range of 5~15km, indicating that the seismogenic layer in the study area is 5~15km deep in the middle and upper crust. 相似文献
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本文通过对重力和航磁资料解译,研究了青藏高原东北部东西向构造特征。在该区域存在6条大型东西向构造带,它们的共同特点是:(1)东西向延伸超过1000km,南北宽约60km;(2)越向深部东西向构造越明显;(3)两条相邻构造带的间距为1°20'',显示等间距分布特征;(4)在大型东西向的构造带之外还有次级东西向构造带存在。青藏高原东北部强震活动与东西向构造有密切的关系,这是由于在北东向主压应力作用下东西向构造左旋剪切运动的结果。 相似文献
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本文采用双差定位方法对云南鲁甸MS6.5地震震后16天的地震序列进行重定位研究.重定位结果显示,主震位于27.11°N,103.35°E,震源深度约15 km;地震序列主要呈“L”形优势分布,分为SSE向和近EW向两支,并均呈现近垂直的震源分布特征,显示此次地震为走滑型,并存在两个不同方向的破裂面.虽然此次地震发生于NE向昭通断裂及其反冲断裂(龙树断裂、大岩洞断裂)附近,但这些断裂均为逆冲型断裂,被排除了作为发震断裂的可能性;鲁甸地震发生在呈放射性分布的多条断裂的交汇部位,SSE向破裂分支与包谷垴断裂的方向一致,近EW向破裂分支与小河断裂南端的走向一致. 鲁甸地震可能已将包谷垴断裂和小河断裂在深部贯通. 相似文献
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1997年9月三水4.4级地震影响场与构造背景 总被引:6,自引:2,他引:4
1997年9月26日广东三水ML4.4级地震以震级小、烈度高、破坏性大为其显著特征;震中位于北东、北西和东西向三组断裂的交汇处附近。对这次地震进行了现场宏观烈度和震害调查,结果表明,极震区呈近东西走向,震中烈度达Ⅵ度。这次地震是东西向断裂活动的结果。 相似文献
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THE STATIC STRESS TRIGGERING INFLUENCES OF THE 2015 MW6.4 PISHAN,XINJIANG EARTHQUAKE ON THE NEIGHBORING AREAS 下载免费PDF全文
Based on the rupture models of the 2015 Pishan MW6.4 earthquake and half space homogeneous elastic model, the Coulomb stress changes generated by the earthquake are calculated on the active faults near the earthquake region. The horizontal stress changes and the displacement field are estimated on the area around the epicenter. Results show that:(1)The Coulomb stress is decreased in the west of the western Kunlun frontal thrust fault(9.5×103Pa), and increased in the east of the western Kunlun frontal thrust fault and the middle of the Kangxiwa faults. More attention should be taken to the seismic rick of the east of the western Kunlun frontal thrust fault; (2)Based on the analysis on the location of the aftershocks, it is found that most of the aftershocks are triggered by the earthquake. In the region of increased Coulomb attraction, the aftershock distribution is more intensive, and in the area of the Coulomb stress reduction, the distribution of aftershocks is relatively sparse; (3)The horizontal area stress increases in the north and south of the earthquake(most part of the Qaidam Basin and the northwest of the Qinghai-Tibet plateau), and decreases in the east and west of the earthquake(northern part of the Qinghai-Tibet plateau and eastern part of the Pamir Mountains). In the epicenter area, the principal compressive stress presents nearly NS direction and the principal extensional stress presents nearly EW direction. The principal compressive stress shows an outward radiation pattern centered on the epicenter with the principal extensional stress along the direction of concentric circles. The principal compressive stress presents NW direction to the west of the epicenter, and NE to the east of the epicenter. With the increase of radius, the stress level gradually decays with 107Pa in the epicenter and hundreds Pa in the Maidan Fault which is in the north of the Qaidam Basin. 相似文献
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兰州地区活动构造的基本特征 总被引:5,自引:0,他引:5
兰州地区发育了NWW向和NWW向2组主导性活动构造带。大致以河口为界,东部地区主要为NWW向的马衔山-兴隆山左旋逆走滑活动断裂系,其新活动明显,是区内的主要控震断裂,1125年兰州7级地震就发生在其中的马衔山北缘断裂带的西端。河口以西为拉脊山北缘断裂和庄浪河断裂等1组NWW向的弧形逆冲断褶带,变形方式以断裂扩展褶皱为主,其新活动可能导致了138年金城-陇西63/4级地震、1440年永登61/4级地震和1995年永登5.8级地震的发生。兰州市区所在的兰州盆地则夹持在上述2组活动构造之间,其内同样发育了NWW向和NWW向的次级断裂,如刘家堡断裂、金城关断裂、雷坛河断裂及深沟桥断裂等,其上具有孕育和发生中强震的构造条件。 相似文献
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