The Study of Paleoearthquakes on the Weihe Fault Zone     

Shi Yaqin  Li Jin  Feng Xijie  Dai Wangqiang  Ren Jun  Li Xiaoni  Dou Mali 《中国地震研究》2008,22(4):470-480

It is indicated by historical records and the exploratory trench on the Weihe fault that the Yaodian-Zhangjiawan segment of the Weihe fault zone has experienced a historical earthquake and 3 paleoearthquake events in the past 9110a. The historical earthquake, namely, event Ⅳ, occurred between 1487 and 1568 AD. The date of paleoseismic event Ⅰ is （9110 ＋ 90） a, and the ages of events Ⅱ and Ⅲ are unknown. The coseismic vertical displacement of events Ⅰ, Ⅱ and Ⅲ is 0.5m, 0.5m and 0.2m, respectively. The exploratory trench also indicates that the Yaodian-Zhangjiawan segment of the Weihe fault was active in the Holocene.  相似文献   

则木河断裂带大箐梁子附近古地震组合探槽研究   总被引：5，自引：1，他引：4  

田勤俭  任治坤  张军龙 《地震地质》2008,30(2):400-411

古地震事件定年具不确定性,为了增加地震事件定年的可信度,文中通过断层活动方式、沉积环境和地震微地貌的综合分析来研究则木河断裂带上的古地震事件。在大箐梁子附近开挖组合探槽,揭露了3次古地震事件,分别距今约160a、3100a和5500～8900a,复发间隔为3000a左右;讨论了与走滑断层型地震相关的沉积过程,揭示了走滑断层在山坡部位形成鼓包和反向陡坎情况下的沉积模式  相似文献   

马尼拉海沟几何形态特征的构造演化意义   总被引：4，自引：0，他引：4  

陈志豪  李家彪  吴自银  吴振利  尚继宏 《海洋地质与第四纪地质》2009,(2)

通过对马尼拉海沟海底地形地貌、构造特征及其相关地震等数据资料的分析,结合俯冲带动力学数值模拟成果,尤其是Schellart等的模式,详细讨论了马尼拉海沟几何形态、海沟南北段俯冲角度突变等构造特征。分析认为,南海中代表古扩张脊的黄岩海山链的俯冲挤入对马尼拉俯冲带的几何形态没有造成较大的影响,其几何形态较符合中等长度(2000～3000km)的海沟模型。由海沟后退和板片反转引起的平行于马尼拉海沟方向的地幔流加剧了海沟南北段俯冲角度的突变。  相似文献   

Serpentinites and serpentinites: Variety of origins and emplacement mechanisms of serpentinite bodies in the California Cordillera          下载免费PDF全文

John Wakabayashi 《Island Arc》2017,26(5)

Most serpentinitized peridotite in orogenic belts is derived from oceanic lithosphere, but the emplacement mechanisms of these rocks vary greatly, as illustrated by the nature of these rock bodies and their contacts. The diverse emplacement mechanisms have important implications for connecting ophiolitic rock occurrences to large‐scale orogenic processes. In the California Cordillera, the largest bodies of ultramafic rocks are parts of ophiolite sheets, such as the Coast Range ophiolite (CRO), that were part of the upper plate of an oceanic subduction system. Such units differ from smaller bodies within subduction complexes such as the Franciscan Complex that were transferred from the subducting plate to the subduction complex during accretion. Some intra‐subduction complex ultramafic rocks occur as nearly block‐free sheets within the Franciscan Complex, and as a part of mafic–ultramafic imbricates or broken formations within the Shoo Fly Complex of the northern Sierra Nevada. Franciscan Complex serpentinite also occurs as sedimentary serpentinite mélange that was partly subducted after deposition in the trench via submarine sliding. Such mélanges include blocks that record older and higher grade metamorphism than the matrix. Sedimentary serpentinite mélange that includes high‐pressure metamorphic blocks is also found in the basal Great Valley Group forearc basin deposits depositionally overlie the CRO. Distinguishing the different serpentinite origins is difficult in the California Cordillera even though a terminal continental collision did not affect this orogenic belt. In more typical orogenic belts with greater post‐subduction disruption, distinction between the types of serpentinite occurrences presents a greater challenge.  相似文献   

某高精密设备平台基础隔振措施分析   总被引：1，自引：1，他引：0       下载免费PDF全文

夏洪春  李晓燕  尹训强 《地震工程学报》2018,40(1):159-165

结合某高精密设备平台基础隔振实际工程,基于UPFs(User Programmable Features)二次开发特点,提出考虑基础-地基-基础动力相互作用计算基础隔振分析的三维有限元方法。该方法首先将动力机器、周围地基以及高精密设备平台基础作为完整的研究对象,通过引入三维紧支黏弹性边界单元模拟半无限地基辐射阻尼效应和远场介质的弹性恢复性能,并在通用有限元软件ANSYS中实现。进而基于最小二乘方法回归分析得到振动衰减关系曲线,通过其与数值分析结果的对比验证计算模型的合理性。最后针对此工程场地条件建立隔振沟减振隔振措施的有限元模型,并对隔振沟影响因素的减振效果进行分析。计算结果表明,隔振沟的位置、深度以及长度是实际工程中需要考虑的重要因素,对其进行合理的选取可获得较好的隔振效果。  相似文献   

Evidence of short-term groundwater recharge signal propagation from the Andes to the central Atacama Desert: a singular spectrum analysis approach   总被引：2，自引：2，他引：0  

Konstantin W. Scheihing 《水文科学杂志》2018,63(8):1255-1261

The effect of pressure-driven groundwater recharge signal propagation in the Andean-Atacamenian environment is investigated by assessing a record of 15 years of water table fluctuations of an unconfined–confined aquifer system. Based on a singular spectrum analysis of water table time series, it is shown that, in the given case, groundwater levels in the central Atacama Desert are hydraulically controlled by two distant recharge areas associated with the Andes. The maximum observed range of the pressure signal propagation is ~50 km over an elevation difference of more than 3000 m at a lag of ~25 months. Several findings indicate that an often-cited study misinterpreted a water level rise at the same site as an in-situ alluvial fan recharge. Thus, the effect’s impact on groundwater dynamics in complex aquifer systems can easily be overlooked. Singular spectrum analysis could be of use to investigate pressure effects at hydrologically comparable sites.  相似文献   

郯庐断裂带安徽明光段紫阳山探槽及其意义     

赵朋  姚大全  郑海刚  杨源源  缪鹏  李军辉  疏鹏 《中国地震》2018,34(4):642-651

郯庐断裂带安徽省内段落属于该断裂带的南段,断裂构造复杂,总体上断层活动性要弱于断裂带的山东、江苏段。近年来笔者多次在苏皖交界地区开展野外地质地貌调查,发现淮河南北两侧的地形地貌存在较大差异。本研究以淮河以南的郯庐断裂带东支断裂明光段为探查重点,在明光紫阳山北侧跨断层开挖地质探槽。探槽(Tc1)显示断层表现为逆冲、张裂等活动形式,且断层向上延伸错动晚第四纪地层;结合年代样品测试结果,表明该段断层晚第四纪以来有较强的活动,最新活动时代可达晚更新世-全新世早期;探槽揭露的断层表现出多种活动形式,显示了明光段断层活动的多期次性和区域构造应力场的复杂性。  相似文献   

基于广义帕累托分布的马尼拉海沟俯冲带地震危险性估计     

田建伟  刘哲  任鲁川 《地震》2017,37(1):158-165

选取马尼拉海沟俯冲带作为潜源区, 基于广义帕累托分布, 通过对一定时段内超过某一阈值的震级数据进行拟合, 建立该潜源区地震危险性估计模型, 估计强震重现水平和震级上限, 并对估计结果的不确定性进行了分析, 得到马尼拉海沟俯冲带震级上限为9.0级, 10 a、 50 a、 100 a、 200 a马尼拉海沟俯冲带的震级重现水平期望值分别为7.1级、 7.6级、 7.7级、 7.9级。  相似文献   

双线地铁运营隔振沟屏障性能研究   总被引：4，自引：3，他引：1       下载免费PDF全文

丁智  张霄  吴敏慧  李丹薇  陈雷越 《地震工程学报》2019,41(1):9-15

为研究双线地铁运营时隔振沟的减振效果,基于2.5维有限元法建立双线地铁列车-轨道-地基土体耦合分析模型。模型克服现有研究将轨道结构简化为弹性地基欧拉梁的缺陷,引入实际钢轨动力学参数,实现双线地铁列车荷载下隔振沟对周围地基的隔振效果分析,比较空沟、填充沟两种不同隔振措施的减振特性,并对填充沟隔振影响因素进行系统的参数分析。研究结果表明:双线运营地铁荷载下,空沟隔振作用体现在沟后范围内,填充沟减振范围更广且效果更好,相比空沟更具工程实用性;填充沟在沟深较小时也能发挥良好的减振作用,增大沟深、沟宽均可有效提高减振效果。研究成果可为今后双线地铁隔振设计与施工提供有益参考。  相似文献   

日本-千岛海沟转折处地震层析成像研究     

郭雨帆  罗佳宏  宫伟  董非非  汤兰荣  查小惠 《大地测量与地球动力学》2018,38(6):639-645

根据P波走时地震数据,使用双差层析成像方法,获得较高分辨率的日本-千岛海沟转折处俯冲带200 km深度内的震源重定位及P波速度结构结果。将日本-千岛海沟转折处俯冲带分为北日本海沟俯冲带及南千岛海沟俯冲带,且200 km深度内太平洋俯冲板块是连续的。最后,结合水深地形数据、断裂特征资料,划分日本-千岛海沟转折处俯冲带的断裂级别。  相似文献