济阳坳陷横波速度研究及应用   总被引：1，自引：0，他引：1  

李红梅  韩文功 《物探与化探》2003,27(5):362-365

随着多波勘探的发展,横波已越来越多地应用在实际勘探生产中,横波速度参数研究对于指导勘探是十分必要的.笔者利用纵横波VSP测井得到的纵横波速度,根据最小平方误差建立的速度模型,建立了济阳坳陷的纵波、横波、转换波速度参数,应用转换波速度参数提高了盐家地区的多波资料解释精度;利用多种资料总结出纵横波速度关系,为本区今后开展多波勘探提供基础资料.  相似文献   

随机地震动模拟的时间序列法及其工程应用   总被引：3，自引：0，他引：3  

胡孔国  陈小兵  岳清瑞 《世界地震工程》2003,19(1):141-153

系统研究了AR和ARMA时间序列方法生成给定加速度功率谱人工地震波的新方法，根据相应理论编制了程序，并生成了人工地震加速时程曲线，然后用生成的人工地震波进行结构动力时程分析，与实际地震波分析的结果进行了对比，计算结果表明，本文用于合成人工地震波的方法是可行的，生成的人工波可以用于实际结构的地震反应分析。  相似文献   

基于脉冲频响函数的MATLAB动力方程求解方法   总被引：3，自引：0，他引：3  

马乐为  吴敏哲  谢异同 《世界地震工程》2003,19(2):168-171

提出一种基于脉冲频响函数并利用MATLAB求解的方法，由于脉冲频响函数利用卷积公式进行动力微分方法计算，因此，从理论上讲，它适合于任意外力下的动力方程求解，同时，MATAL又提供了卷积函数conv，所以，在MATLAB下求解动力方程将变得十分容易。  相似文献   

最不利地震动在网壳结构抗震设计中的应用   总被引：3，自引：0，他引：3  

范峰  钱宏亮  谢礼立 《世界地震工程》2003,19(3):17-21

利用文献提供的最不利地震动，对网壳结构等大跨空间结构进行了分析，分别考察了仅水平输入和三向地震波输入的两种情况，对最不利地震动在网壳结构抗震设计中的适用性进行了探讨，并在一实际工程设计中进行了应用。大跨度空间结构在水平地震动输入时，宜按照的最不利地震动进行设计；在三向地震动同时输入时，应同时分别按所推荐最不利设计地震动和按常规选用的地震动，对大跨度空间结构进行抗震分析。  相似文献   

Study of crustal structure with S—wave data from Maqen—Jingbian profile     

刘宝峰  李松林  张先康  张成科  任青芳  海燕 《地震学报(英文版)》2003,16(1):92-98

2-D crustal velocity structure and vp/vs are obtained by processing and interpretation of S-wave data from Maqen-Jingbian deep seismic sounding(DSS)profile.The result shows that there exist obvious differences in 2-D S-wave velocity structure and vp/vs ratio structure along the profile.The S-wave velocities are low and vp/vs ration is high for the westem section of the profile and Haiyuan region,while they are normal for the middle and eastern sections.The changes in lithologic characters of two major anomalous zones are discussed according to lateral variation of S-wave velocity structure and vp/vs ratio structure.It is concluded that the development and occurrence of the Haiyuan strong earthquake is not only related to tectonic activities,but also to lithologic characters of the region.  相似文献   

Compression of the North Hemisphere derived from space geodesy     

金双根  朱文耀 《地震学报(英文版)》2003,16(1):99-106

Introduction With the development of global tectonics and overall detections for global tectonics with multi-geophysical methods, ones can roundly study on the geological tectonics of sampling and magnetic stripe image, so as to summarize and interpret the geometrical and kinematical charac-teristics for the distribution of the ocean and the land, and spreading state of the global tectonics in a global scale. From a comprehensive view, the South and North hemispheres are clearly unsym-metrical…  相似文献   

酒钢黑沟矿爆破效应研究     

苏宏伟 《高原地震》2003,15(1):51-54

利用爆破记录的原始资料，计算出地动位移、振动速度，然后确定K、α值。根据不同建筑物的安全振动速度，给出安全爆破的最大Q(炸药量)的参考值。  相似文献   

Crustal structure beneath the Songpan—Garze orogenic belt   总被引：2，自引：0，他引：2  

王椿镛  韩渭宾  吴建平  楼海  白志明 《地震学报(英文版)》2003,16(3):237-250

The Benzilan-Tangke deepseismic sounding profile in the western Sichuan region passes through the Song-pan-Garze orogenic belt with trend of NNE.Based on the travel times and the related amplitudes of phases in the record sections,the 2-D P-wave crustal structure was ascertained in this paper.The velocity structure has quite strong lateral variation along the profile.The crust is divided into 5layers,where the first,second and third layer belong to the upper crust,the forth and fifth layer belong to the lower crust.The low velocity anomaly zone gener-ally exists in the central part of the upper crust on the profile,and it integrates into the overlying low velocity basement in the area to the north of Ma‘erkang.The crustal structure in the section can be divided into 4parts:in the south of Garze-litang fault,between Garze-Litang fault and Xianshuihe fault,between Xianshuihe fault and Longriba fault and in the north of Longriba fault,which are basically coincided with the regional tectonics division.The crustal thickness decreases from southwest to northeast along the profile,that is ,from62km in the region of the Jinshajiang River to 52km in the region of the Yellow River.The Moho discontinuity does not obviously change across the Xianshuihe fault basesd on the PmP phase analysis.The crustal average velocity along the profile is lower,about 6.30 km/s.The Benzilan-Tangke profile reveals that the crust in the study area is orogenic.The Xianshuihe fault belt is located in the central part of the profile,and the velocity is positive anomaly on the upper crust,and negative anomaly on the lower crust and upper mantle.It is considered as a deep tectonhic setting in favor of strong earthquake‘s accumulation and occurrence.  相似文献   

Exploration and Study on Deep Crust Structural Characteristics in the Jiashi-Artux Seismic Region     

Zhao Jinren  Zhang Xiankang  Zhang Chengke  Ren Qingfang  Cheng Shuangxi  Zhang Jianshi  Nie Wenying  PAN Shuzhen 《中国地震研究》2003,17(2):103-112

The data from two deep seismic sounding profiles was processed and studied comprehensively. The results show that crnst-mantle structures in the investigated region obviously display layered characteristics and velocity structures and tectonic features have larger distinction in different geological structure blocks. The boundary interface C between the upper and lower crust and Moho fluctuate greatly. The shallowest depths of C (30.0km) and Moho (45.5km) under Jiashi deepen sharply from Jiashi to the western Kunlun mountain areas, where the depths of C and Moho are 44.0km and 70.0km, respectively. The higher velocity structures in the Tarim massif determine its relatively “stable“ characteristics in crust tectonics. The phenomenon in the Jiashi region, where the distribution of earthquake foci mostly range from 20kin to 40kin in depth, may infer that the local uplift of C and Moho interface, anomalonsly lower velocity bodies and deep large faults control earthquake occurrence and seismogenic processes in the Jiashi strong earthquake swarm.  相似文献   

非开挖导向钻进实际轨迹的控制设计   总被引：4，自引：0，他引：4  

张德龙  蒋荣庆 《吉林大学学报(地球科学版)》2003,33(2):246-248

非开挖导向钻进技术，具有施工速度快、适用范围广等优点，得到了广泛的应用。在实际钻进中，由于钻进在地下的不确定性，影响了导向钻进的顺利进行。到得钻进中当前点的顶角、方位角和孔深，通过均角全距法原理，可以近似地描绘出当前钻孔的空间实际轨迹，并确定钻头的位置。应用这一原理，同时运用VisualBasic语言和AutoCAD绘图工具相结合的方法，编制一套应用程序，可以直接绘制出当前钻孔轨迹，并可实现对钻孔轨迹的调控，从而保证导向钻进的顺利进行。  相似文献