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141.
142.
对帕米尔东缘区域中深源地震与浅源地震进行波形对比,并使用交切法和Hyposat地震定位方法进行地震定位对比,从不同角度探讨该区域中深源地震特征. 相似文献
143.
为了减少闪电对人类生命财产和各种电子设备造成的损失,同时研究雷暴活动的形成机制,并为闪电监测预警提供技术支持,开展闪电定位算法研究具有重要意义。闪电发生时辐射从极低频到甚高频范围的电磁脉冲,通过闪电定位系统获取闪电辐射源脉冲信号参数便可定位闪电。概述了闪电定位原理及基本方法,比较了基于空间谱估计的Capon算法、MUSIC算法及2种改良算法,介绍了基于均匀圆阵的二维MUSIC算法。采用Matlab分析了这几种闪电定位算法的性能,最后提出二维修正MUSIC算法,为闪电定位系统提供坚实的理论依据。 相似文献
144.
Tomoyoshi Takeuchi 《Marine Geodesy》2013,36(3-4):225-231
Abstract It is desired to track the location of an underwater data collecting platform using acoustic range data. A long‐range and high‐resolution acoustic system for underwater locating has been investigated. The system provides continuous and highly accurate tracking of a platform referenced to bottom‐mounted buoys. Each reference buoy contains an acoustic transponder, which is used to obtain ranging data from the transponder to the platform. The transponder has a signal source that is phase‐modulated by a maximal‐length binary sequence and a correlation processing unit to be capable of detecting received acoustic signals with high SNR in a noisy environment or in attenuation due to long‐range propagation, and to identify multipath acoustic signals. The acoustic system has been designed and sea tests tried. The results of that experiment have yielded capability of a submeter underwater acoustic positioning system. 相似文献
145.
146.
湘中锑矿带断裂体系分维及其对成矿流体运移和矿床定位的指示作用 总被引:7,自引:0,他引:7
根据分形理论计算了湘中各锑矿带断裂体系的计盒维数和信息维数。通过对各矿带断裂体系分维特征与锑矿分布之间关系的分析,发现断裂体系的分维高值区与锑矿分布密集区相对应,这不仅表明断裂是成矿流体运移的主要通道,同时也表明断裂体系分维特征是定量描述锑矿床定位及成矿流体运移,聚集条件的一个重要参数。 相似文献
147.
Locating an earthquakes focal depth is always a key project in seismology. Precise focal depth is of critical importance for evaluating seismic hazards, deciphering dynamic mechanisms of earthquake generating,estimating aftershock evolutions and risk,as well as monitoring nuclear tests. However,how we determine an accurate focal depth is always a challenge in seismological studies. Aiming to solve these problems, we analyzed and summarized the present status and the future development of earthquake focal depth locating. In this paper we first reviewed the present status of focal depth locating in the world,and summarized the frequently-used relocating methods and ideas at present,and introduced two types of focal depth relocating ideas: arrival time relocating and waveform modeling methods. For these ideas,we systematically described the S-P and the Pn-Pg methods that belong to arrival time method,and polarization focal depth locating and amplitude focal depth locating that belongs to waveform modeling,and further analyzed the advantages and limitations of these methods. Since the depth phase methods are highly sensitive to focal depth,and are relatively free from the uncertainties of crustal models,we mainly reviewed the depth phases of s Pm P,s PL,s Pn,and s Sn,and quantitatively evaluated their availabilities and characteristics. Second,we also discussed the effects of crustal velocity models on the reliability of focal depth locating,and reviewed the advancements of seismic tomography techniques over recent years. Finally,based on the present status of the progress on the focal depth locating,and studies of seismic velocity structures,we proposed an idea of combining multiple datasets and relocating methods,jointly utilizing seismologic and geodetic techniques to relocate focal depth,which should be the major research field in investigating focal depth and source parameters in the near future. 相似文献
148.
实际海面受风浪的影响是个随机起伏的复杂曲面.一个随机起伏的自由表面对地震波形成相当复杂的散射,进而影响波场在靶区的二次照明与成像结果;此外,起伏海面具有小尺度随机起伏的特性,难以用贴体网格等处理大尺度起伏地表的常规方法和技术对其进行逼近和处理.鉴于此,利用不等距有限差分法实现小尺度起伏海面的波场自由表面边界条件,以此进行正演、波场照明分析;利用逆时偏移(Reverse Time Migration,RTM)进行起伏海面下的成像并对成像结果进行分析.不同模型的试算结果表明:起伏海面引起的复杂散射使靶区地下照明不均匀、成像界面发生弯曲和畸变,从而降低成像结果的分辨率和信噪比. 相似文献
149.