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根据地震动态触发理论,计算了2000年苏门答腊MS8.0,地震在缅甸MS6.5地震破裂面上产生的动态库仑应力:正峰值为1.357 5 MPa,负峰值为-1.113 5 MPa。峰值大于地震触发阈值0.01 MPa,苏门答腊地震的发生对缅甸地震具有一定的触发作用。在计算过程中发现,主震基本参数、传播过程中介质参数和被触发地震断层参数的准确性对计算结果有较大影响。 相似文献
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在郯庐断裂带安徽段由北向南分别于泗县、明光、肥东、桐城布设了4个测区,每个测区各布设了4条跨断层土壤气测量剖面,测量土壤气Rn、Hg和CO_2的浓度。根据16条跨断层土壤气剖面的测量结果,对郯庐断裂带安徽段的3种土壤气体的释放特征及其与断层空间位置间的关系进行了初步分析。结果表明,气体在断裂带附近较为富集,对断层位置有一定指示作用;气体的富集程度与断裂的活动性、该区段断层岩性及地质环境有一定关系。该结果对于认识测量区域气体的积累特征及构造地球化学研究有一定意义。 相似文献
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New Activity of the Tanlu Fault Zone in the South of Huaihe to the Nvshanhu Segment since the Late Quaternary 
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下载免费PDF全文 Yao Daquan Zheng Haigang Zhao Peng Yang Yuanyuan Wang Xingzhou Miao Peng Fang Zhen Tao Yuechao Li Junhui Wang Jun Wang Xiaoli 《中国地震研究》2017,31(2):225-233
Taking the Huaihe to the Nvshanhu segment of the Tanlu (Tancheng-Lujiang) fault zone as the main research target to explore whether there has been new activity since the late Quaternary, and based on the interpretation of remote sensing images and repeated surface investigations, we excavated trenches at the sections where the tectonic landform is significant, identified and recorded the deformation patterns of the fault and analyzed the activity behavior. Samples of new activity and deformation were collected and oriented slices were ground based on the samples'' original state to make the micro structural analysis and demonstration. All of the above research shows very clear linear tectonic geomorphology along the fault, three trenches across the fault zone all revealed new deformation traces since late Quaternary. The latest stratum dislocated by the fault is the late Quaternary and Holocene. The main slip mode is stick slip, as represented typically by fault scarps, wedge accumulation, the faults and the filled cracks and so on. In general, it shows the characteristics of brittle high-speed deformation and belongs to the prehistoric earthquake ruins. The above understanding was confirmed partially by microscopic analysis. In addition, the similarities and differences and the possible reasons for the characteristics of the latest activities of the Tancheng-Lujiang fault zone in the north and south of the Huaihe River regions are also discussed in this paper. 相似文献
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郯庐断裂带南段淮河至女山湖段落已被证实具有晚第四纪活动性，为进一步追踪断裂带在女山湖以南的活动情况，选取明光至定远池河镇段落进行遥感解译、地质地貌调查、探槽开挖及年代样品测试等工作。研究发现，该段断裂在卫星影像上显示线性特征较差，发育断裂主要为池河-太湖断裂；断裂新活动主要表现为控制池河河谷的发育及沿明南土山村、池河石塘岳、池河周王等地展布的线性岗状地貌；在上述岗地边缘开挖探槽揭示断裂在该段最新活动方式具挤压逆冲性质，最新活动时代为中更新世，晚更新世以来不活动。上述结果初步表明，该段与其北侧相邻的淮河至女山湖段在第四纪活动性上存在差异，可能为郯庐断裂带在女山湖附近存在分段导致。 相似文献
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以郯庐断裂带淮河南到女山湖段晚第四纪以来是否具有新活动为主要研究目标,通过遥感影像资料解译及地表反复调查,选择构造地貌显著地段开挖探槽,识别和记录其变形形态,分析其活动习性,定向采集新活动变形物质,在保持原态基础上磨制定向薄片,并进行微观构造分析论证。研究表明,断裂沿线线状构造地貌清晰,横跨断裂带的3个探槽均揭示出晚第四纪以来活动痕迹,断裂最新错断了晚更新世-全新世地层;滑移方式多表现为粘滑,典型表现为断层陡坎、楔状堆积、断层和充填裂缝等,总体显示为脆性高速变形特征,属于史前地震遗迹。上述认识部分得到微观分析证实。文中还初步探讨了淮河南北郯庐断裂最新活动特征的异同点及其可能的原因。 相似文献
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Because of quick development of cities, the update of urban GIS data is very important. Change detection is the base of automatic or semi-automatic data update. One way of change detections in urban area is based on old and new aerial images acquired in different durations. The corresponding theory and experiments are introduced and analyzed in this paper. The main procedure includes four stages. The new and old images have to be registered firstly. Then image matching, based on the maximum correlation coefficient, is performed between registered images after the low contrast areas have been removed. The regions with low matching quality are extracted as candidate changed areas. Thirdly, the Gaussian-Laplacian operator is used to detect edges in candidate changed areas on both the registered images, and the straight lines are detected by Hough transformation. Finally, the changed houses and roads can be detected on the basis of straight line matching in candidate changed areas between registered images. Some experimental results show that the method introduced in this paper is effective. 相似文献
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ZHANG Jianqing ZHANG Zuxun FANG Zhen FAN Hong ZHANG Jianqing Professor National Laboratory 《地球空间信息科学学报》1999,2(1):16-20
Because of quick development of cities, the update of urban GIS data is very important. Change detection is the base of automatic or semi-automatic data update. One way of change detections in urban area is based on old and new aerial images acquired in different durations. The corresponding theory and experiments are introduced and analyzed in this paper. The main procedure includes four stages. The new and old images have to be registered firstly. Then image matching, based on the maximum correlation coefficient, is performed between registered images after the low contrast areas have been removed. The regions with low matching quality are extracted as candidate changed areas. Thirdly, the Gaussian-Laplacian operator is used to detect edges in candidate changed areas on both the registered images, and the straight lines are detected by Hough transformation. Finally, the changed houses and roads can be detected on the basis of straight line matching in candidate changed areas between registered images. 相似文献
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针对2014年8月—2015年1月安徽金寨发生的M_L3.9震群,利用匹配滤波技术补充台网目录遗漏的地震事件,再利用波形互相关震相检测技术标定P波和S波到时,进一步采用双差定位方法对震群进行重定位,结合震源机制解等分析此次震群活动可能的发震构造。计算结果显示,通过互相关扫描检测到1376个地震台网常规分析遗漏的地震,数量约为台网目录给出的585个事件的2.35倍。检测到的遗漏地震震级估算为M_L0～2.3,通过震级-频次统计分析,加入遗漏地震后地震目录的完整性在M_L0～1.5范围内有较明显的改善。重定位后地震走时残差更小,水平位置更集中,沿NNE向断裂F和NW向青山-晓天断裂呈现近直立的条带状分布。结合地质构造、震源机制解和水库因素,推测2014年金寨M_L3.9震群可能是由周边水库水下渗引起NW向青山-晓天断裂与NNE向断裂F慢滑动而触发的。 相似文献
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