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1.
南京河西地区设计地震动研究 总被引：7，自引：3，他引：4
本文根据南京及周围地区的地震环境,采用概率法对南京河西地区某高层公寓工程场址进行了地震危险性分析,采用等效线性化模型考虑场地土的非线性特性的影响,并用一维波动模型进行了场址土层地震反应和场地地震动效应分析,给出了５０年超越概率６３％,１０％和３％的场址基岩和地表的水平向加速度反应谱值加速度。 相似文献
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《世界地震工程》2017,(4)
建筑物振动特性对于结构抗震设计有重要的理论价值,其中自振周期和阻尼比是2个主要的动力参数。对福州地区129栋不同高度钢筋混凝土建筑物进行振动测试,并统计建筑物的基本特征,研究了高度在21~99m范围内建筑物的自振周期和阻尼比随建筑物高度变化的规律。结果表明:建筑物自振周期随高度增加而增大,有良好的相关性,自振周期约是高度的0.018 63倍;长短轴向自振周期也随高度的增加而增大,长轴向自振周期约是高度的0.014 56倍,短轴向自振周期约是高度的0.018 46倍;随着建筑物高度的增大,阻尼比、长轴向阻尼比和短轴向阻尼比这三者在一定的范围内近似均匀分布,对高度的敏感性低,其中建筑物阻尼比的平均值为4.44%,与建筑抗震设计规范所取的定值5%是比较接近的。研究结论:可为蓬勃发展的高层钢筋混凝土建筑物的初期设计提供科学依据。 相似文献
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当前地震动速度时程时域特性分析方法,仅能分析岩溶区地震动速度时程的振动周期、强弱程度与时间变动的问题,但未能准确计算岩溶区砌体建筑物自振频率,导致砌体建筑环境振动特性分析结果存在误差。深入研究岩溶区砌体建筑环境振动特性分析方法,构建混凝土损伤塑性模型,分析岩溶区砌体建筑材料的屈服(受压)应力-非弹性应变关系、开裂(受拉)应力-非弹性应变关系和损伤因子;采用贝叶斯方法检测岩溶区砌体建筑受压受拉时的自振频率,通过L-M神经网络法消除自振频率后,使用振动特性分析方法准确分析岩溶区砌体建筑环境振动特性。实验结果表明,所提方法分析准确率高达0.99,分析16栋岩溶区砌体建筑环境振动特性耗时仅有5 ms,具有较高的分析精度和效率。 相似文献
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对昆明16栋典型钢筋混凝土高层建筑物的振动特征(包括建筑物的固有频率、振型和阻尼比)进行观测与分析,对地震响应数值模拟研究,获取实测高层建筑物第一至第三振型及结构,计算第一至第二振型自振周期结果,采用数学线性回归方法,模拟得到昆明高(超高)层建筑结构实测第一至三振型和计算第一至第二振型周期公式,为类似建筑结构的设计提供经验和依据. 相似文献
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软土地基深开挖对场的设计地震动的影响 总被引：1，自引：0，他引：1
本文根据南京河西地区所处的地震地质环境,地震活动环境及其岩地震动衰 减规律,在场址区地震危险性分析基础上确定该地区的基岩地震动参数,并选取河西地区某个典型工程场地,根据场地土的静、动力性能参数的测试结果,进行场地土层地震反应分析,研究软土地基条件下地基深开挖场地的地震动效应及其对场地设计地震动参数的影响。文中给出了设计基准为５０年及１００年时对应不同抗震高防水准的设计地震动参数,该结果对河西地区其 相似文献
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软土地基深开挖对场地设计地震动的影响 总被引：16，自引：3，他引：13
本文根据南京河西地区所处的地震地质环境、地震活动环境及基岩地震动衰减规律,在场址区地震危险性分析基础上确定该地区的基岩地震动参数,并选取河西地区某个典型工程场地,根据场地上的静、动力性能参数的测试结果,进行场地上层地震反应分析,研究软土地基条件下地基深开挖场地的地震动效应及其对场地设计地震动参数的影响．文中给出了设计基准期为５０年及１００年时对应不同抗震设防水准的设计地震动参数,该结果对河西地区其它高层建筑的抗震设计也有一定的参考价值． 相似文献
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以抗震设防7度区的某高层钢框架结构建筑为研究对象,研究基于隔震就位连接技术的高层钢框架结构建筑抗震技术。对研究对象采用抗震就位连接技术,通过在隔震层中设置弹性滑板支座、厚层橡胶隔震支座化黏滞阻尼器等隔震装置提升研究对象自振周期,降低其上部结构受地震作用的影响程度,增强抗震性能。对研究对象进行模态分析与时程分析,结果显示,所研究隔震技术在显著提升研究对象自振周期,使其摆脱场地特征周期的同时,也能够延缓扭转振型的形成,显著降低地震作用对研究对象上部结构的影响,说明所研究技术的运用具有较好的抗震效果。 相似文献
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为了分析一次性爆破拆除多栋建筑造成的地面振动的特征及对周边建筑物的影响,对武汉交通学校群楼爆破拆除中的地面振动进行了测量,并对实测的塌落振动的峰值、频谱特性进行分析。结果表明:此次监测记录到的峰值频率在5～10 Hz,对比高架桥以及单一高层结构爆破拆除数据,倒塌叠加使得振动能量在频谱上分布更加离散,其峰值频率与周边结构自振频率相差变大,周边建筑共振的危险性降低;对于周围的结构而言,水平振动持时大于竖向振动,但水平振动幅值明显小于竖向振动;爆破塌落振动的竖向分量对周围结构的威胁较大,应采取有效的缓冲及隔振措施;由《爆破安全规程》和周边建筑爆破前后主振频率分析可知,本次爆破拆除工作未对周边建筑造成破坏性影响,验证了群楼爆破拆除方案的高效性和安全性。 相似文献
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《震灾防御技术》2022,17(4):682-690
为分析雅安地区场地结构引起的震动特性,选取该地区重大安评项目中的实际测试钻孔进行场地地震反应分析,采用等效线性化方法,并以NGA强震记录为输入,开展场地反应计算,在全面分析该地区场地地震特征的基础上,以峰值速度为参数指标,研究场地条件引起的峰值速度放大效应。研究结果表明,雅安地区场地卓越周期约为0.2 s,自振周期为0.2 s的建筑结构破坏相对严重;随着基岩峰值加速度的增大,峰值速度呈增大趋势,峰值速度与峰值加速度变化趋势并非完全一致,分析场地效应时应考虑多种地震动参数的变化规律;不同地震输入下峰值速度放大系数为1～1.8;峰值速度放大系数kv在不同强度基岩输入下,大致呈随等效剪切波速的增大而减小的趋势,软土场地更易引起场地峰值速度的放大,这种现象在芦山地震中较为明显。 相似文献
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九十年代北祁连河西地区重力场变化特征 总被引：2，自引：0，他引：2
以１９８９￣１９９７年北祁连河西地区流动重力监测资料为基础,分为１９８９￣１９９１、１９９１￣１９９５、１９９５￣１９９７年三个时段,定性定量分析了这三个时段该地区重力的时空变化特征,得出了北祁连河西地区的重力场现处于祁连山重力值上升、河西走廊重力下降的逆继承性重力变化的结论。 相似文献
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基于地震剖面解释的构造分析表明，河西走廊西段及邻区发育有许多晚第三纪-第四纪的逆断层与走滑断层. 其主要类型有两种:一是与北祁连逆冲推覆作用有关的南倾逆断层，其走向北西，主要分布于北祁连山东北缘及河西走廊西南部地区；二是与阿尔金断裂活动有关的逆断层与走滑断层，主要分布于红柳峡、宽台山——合黎山地区. 这些断层与新生代始新世末期以来印-藏碰撞的远距离效应有关. 它们于晚第三纪开始活动，主要活动于第四纪时期，而且大多目前仍在活动，属于活动性断层，是河西走廊地区地震的潜发因素. 此外，它们还造成了地层的强烈变形，形成了一系列的地貌阶地和河流的水平错移. 相似文献
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PRESENT KINEMATICS CHARACTERISTICS OF THE NORTHERN YUMUSHAN ACTIVE FAULT AND ITS RESPONSE TO THE NORTHEASTWARD GROWTH OF THE TIBETAN PLATEAU 
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下载免费PDF全文 CHEN Gan ZHENG Wen-jun WANG Xu-long ZHANG Pei-zhen XIONG Jian-guo YU Jin-xing LIU Xing-wang BI Hai-yun LIU Jin-rui AI Ming 《地震地质》2017,39(5):871-888
Qilian Shan and Hexi Corridor, located in the north of Tibetan plateau, are the margin of Tibetan plateau's tectonic deformation and pushing. Its internal deformations and activities can greatly conserve the extension process and characteristics of the Plateau. The research of Qilian Shan and Hexi Corridor consequentially plays a significant role in understanding tectonic deformation mechanism of Tibetan plateau. The northern Yumushan Fault, located in the middle of the northern Qilian Shan thrust belt, is a significant component of Qilian Shan thrust belt which divides Yumushan and intramontane basins in Hexi Corridor. Carrying out the research of Yumushan Fault will help explain the kinematics characteristics of the northern Yumushan active fault and its response to the northeastward growth of the Tibetan plateau.Because of limited technology conditions of the time, different research emphases and some other reasons, previous research results differ dramatically. This paper summarizes the last 20 years researches from the perspectives of fault slip rates, paleao-earthquake characteristics and tectonic deformation. Using aerial-photo morphological analysis, field investigation, optical simulated luminescence(OSL)dating of alluvial surfaces and topographic profiles, we calculate the vertical slip rate and strike-slip rate at the typical site in the northern Yumushan Fault, which is(0.55±0.15)mm/a and(0.95±0.11), respectively. On the controversial problems, namely "the Luotuo(Camel)city scarp" and the 180 A.D. Biaoshi earthquake, we use aerial-photo analysis, particular field investigation and typical profile dating. We concluded that "Luotuo city scarp" is the ruin of ancient diversion works rather than the fault scarp of the 180 A.D. Biaoshi earthquake. Combining the topographic profiles of the mountain range with fault characteristics, we believe Yumu Shan is a part of Qilian Shan. The uplift of Yumu Shan is the result of Qilian Shan and Yumu Shan itself pushing northwards. Topographic profile along the crest of the Yumu Shan illustrates the decrease from its center to the tips, which is similar to the vertical slip rates and the height of fault scarp. These show that Yumu Shan is controlled by fault extension and grows laterally and vertically. At present, fault activities are still concentrated near the north foot of Yumu Shan, and the mountain ranges continue to rise since late Cenozoic. 相似文献
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通过室内航片判读和野外调查 ,在酒西盆地发现 3条全新世活动逆掩断层 ,它们全新世以来的垂直活动速率都很接近 ,为 0 18～ 0 2 5mm/a。通过探槽揭露出的 3条断层全新世以来各发生两次古地震事件。根据探槽揭露的古地震年代及断层活动所形成的微地貌特征分析 ,阴洼山断层是独立活动的 ;北大河断层和新民堡断层上的古地震事件在时间上可能非常接近 ,具有丛集特征 ,或者是一次地震事件分别破裂这两条断层 ,但目前的测年手段还无法区别它们是一次破裂事件形成还是时间上非常接近的两次事件所形成的 相似文献
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Introduction Hexi Corridor, a corridor extended over 1 000 km and with a strike of WNW-ESE, is locatedbetween Alxa uplift and northern Qilianshan Caledonian folding belt of northern Qinghai-Xizang(Tibet) Plateau (Figure 1). In the paper, we will discuss the regions between Altun fault and Yu-mushan of the western Hexi Corridor, where the climate is arid, which results in sparse vegetation,but abundant oil and gas resource, and being one of the most important petroleum industry base… 相似文献
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LATE QUATERNARY SINISTRAL STRIKE-SLIP ACTIVITIES OF SANWEI SHAN FAULT IN THE NORTH OF TIBETAN PLATEAU 下载免费PDF全文
下载免费PDF全文 Sanwei Shan Fault is located in the north of Tibet, which is a branch of eastern segment of Altyn Tagn fault zone. This fault is distributed along the boundary of fault facet and the Quaternary, with the total length of almost 150km. The fault is a straight-line structure read from the satellite image. Based on the spatial distribution of the fault, three segments are divided, namely, Xishuigou-Dongshuigou segment, Dongshuigou-West Shigongkouzi segment and West Shigongkouzi-Suangta segment, these three segments are distributed by left or right step.Though field microgeomorphology investigation along Sanwei Shan Fault, it has been found that two periods of alluvial-pluvial fans are distributed in front of Sanwei Shan Mountain, most of which are overstepped. Comparing the distribution of alluvial-pluvial fans with their formation age in the surrounding regions, and meanwhile, taking the results of optical stimulated luminescence(OSL) dating, it's considered that the formation age of the older alluvial-pluvial fans, which are distributed in northern Qilian Shan, inside of Hexi Corridor and western Hexi Corridor(including the Sanwei Shan piedmont fans), is between later period of late Quaternary and earlier period of Holocene. The gullies on the older fan and ridges have been cut synchronously. The maximum and minimum sinistral displacement is 5.5m and 1.7m, but majority of the values is between 3.0~4.5m. Taking the results from the OSL dating, we conclude that the minimum sinistral strike-slip rate is(0.33±0.04) mm/a since 14 ka BP and(0.28±0.03) mm/a since 20 ka BP. 相似文献
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总结了1993～1997年应用模糊聚类分析方法对甘肃省地震预报的效果,通过评价得到对河西走廊地区和南北地震带北段地区的预报能力分别为0．55和0．61,扣除随机概率的预报成功率分别为0．5和0．58。 相似文献
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Late Cenozoic sediments in the Hexi Corridor, foreland depression of the Qilian Mountain preserved reliable records on the evolution of the Northern Tibetan Plateau. Detailed magnetic polarity dating on a 1150 m section at Wenshushan anticline in the Jiudong Basin, west of Hexi Corridor finds that the ages of the Getanggou Formation, Niugetao Formation and Yumen Conglomerate are >11-8.6 Ma, 8.6-4.5 Ma and 4.5-0.9 Ma respectively. Accompanying sedimentary analysis on the same section suggests that the northern Tibetan Plateau might begin gradual uplift since 8.6-7.6 Ma, earlier than the northeastern Tibetan Plateau but does not suppose that the plateau has reached its maximum elevation at that time. The commencement of the Yumen Conglomerate indicates the intensive tectonic uplift since about 4.5 Ma.
相似文献20.
《中国科学:地球科学(英文版)》2021,(3)
Landscape evolution models(LEMs) are essential tools for analyzing tectonic-climate interactions and reproducing landform-shaping processes. In this study we used a LEM to simulate the evolution of the mountains from the central Hexi Corridor in the northeastern Tibetan Plateau, where the climate is arid and the surface processes are relatively uniform. However,there are pronounced differences in the topography between the mountains around the central Hexi Corridor. The East Jintanan Shan, West Jintanan Shan and Heli Shan are located in the northern part of the corridor; and the Yumu Shan in the southern part.Firstly, several representative areas were selected from these mountains to analyze the topographic characteristics, including the uniform valley spacing, local relief, and the outlet number. Secondly, a LEM for these areas was constructed using the Landlab platform, and the landscape evolution was simulated. With uniform valley spacing and other topographic characteristics as the criteria, we compared the realistic and simulated terrain for different model ages. Finally, based on the similarity of the simulated and realistic terrain, we estimated the timing of the initial uplift and the uplift rate of the four mountain ranges. The results are consistent with previous geological and geomorphological records from these youthful stage mountains that have not yet reached a steady state. Our findings demonstrate that LEMs combined with topographic characteristics are a reliable means of constraining the timing of the initial uplift and the uplift rate of the youthful stage mountain. Our approach can potentially be applied to other youthful stage mountains and it may become a valuable tool in tectonic geomorphology research. 相似文献