Hilbert-Huang变换在提取阵列声波信号动力特性中的应用   总被引：5，自引：3，他引：2       下载免费PDF全文

王祝文  刘菁华  聂春燕 《地球物理学进展》2008,23(2):450-455

阵列声波信号是典型的非线性、非平稳信号,其动力特性的量化提取对于进行地层结构构造分析提供了必要的基础资料.而Hilbert-Huang变换(HHT)是一种处理非线性、非平稳信号的新方法.它通过经验模态分解(EMD)将信号分解为有限个固有模态函数(IMF),并对每个固有模态函数进行Hilbert变换得到Hilbert谱.本文将这种方法应用于阵列声波信号动力特性的提取,有效地获得了信号能量的时频分布,瞬时能量、Hilbert能量、最大振幅对应的时频分布等动力特性,显示了HHT的优势以及对于进一步实现地层结构构造分析的重要意义.  相似文献   

海流剖面仪信号处理系统中最小二乘改进算法的应用研究     

朱昊  刘文耀  梁捷  郝永杰 《海洋技术学报》2004,23(3):41-45

ADCP技术是海洋测流领域的热门技术,而频谱估计方法的研究是该技术的核心。文章介绍一种最小二乘的改进算法(ELMS),利用该算法可以很好的提取出淹没在白噪声下的正弦频谱。和传统的快速傅立叶变换方法(FFT)相比,该算法极大的压缩了数据量的要求,而且在信噪比为0DB的时候,仍能够较准确的估计出信号的谱峰位置。实验结果辩明该算法具有良好的鲁棒性。  相似文献   

希尔伯特—黄变换在地电阻率数据处理中的应用     

张国清  高立新  戴勇  杨彦明  格根 《地震地磁观测与研究》2017,38(3):81-87

希尔伯特—黄变换用于处理非线性非平稳信号,由经验模态分解和希尔伯特谱分析2部分组成。本文采用希尔伯特—黄变换方法,相继对大同地震台地电阻率月值数据和宝昌地震台地电阻率月值、整点值数据进行处理。结果显示:(1)大同、宝昌地震台地电阻率月值数据对应的Hilbert谱具有较高分辨率,高幅值在归一化频率0.05—0.15区间内呈"余弦"变化形态;(2)希尔伯特—黄变换在提取地电阻率异常变化、高频信息及去除噪声等方面效果较好,在未来地电资料处理中具有广泛的应用前景。  相似文献   

湍流大气的像质衰减参数及测量     

刘忠 《天文研究与技术》1998,(1)

讨论了经过大气后天文图象的象质衰减,研究了对这种衰减进行描述的视宁度参数ｒ０及其它几个大气光学参数,介绍了几种测量象质衰减参数的方法,重点介绍了我们将差分像运动法运用于白日视宁度测量的尝试以及新设计的可兼顾昼夜的视宁度测量仪,仪器已用于云台白日的视宁度测量。最后对近场近似假设进行了定量分析,在此基础上给出了新确定的近场近似成立的范围,这一范围比以前所给的要更大些。  相似文献   

Hilbert-Huang�任�ڹ��峱�����е�Ӧ��   总被引：3，自引：2，他引：1  

陈涛  李正媛  陈志遥  吕品姬  赵兵  林穗平 《大地测量与地球动力学》2009,29(4):131-134

??(HHT) Hilbert??Huang????????????б???峱??????????????????????????????б????????????????Hilbert?任????????????Hilbert???  相似文献   

Segmentation and differential post-rift uplift at the Angola margin as recorded by the transform-rifted Benguela and oblique-to-orthogonal-rifted Kwanza basins   总被引：1，自引：0，他引：1  

M. Guiraud  A. Buta-Neto  D. Quesne 《Marine and Petroleum Geology》2010

We analyse tectonic and sedimentary field and subsurface data for the Angola onshore margin together with free-air gravity anomaly data for the offshore margin. This enables us to characterize the mode of syn-rift tectonism inherited from the Precambrian and its impact on the segmentation of the Angola margin. We illustrate that segmentation by the progressive transition from the Benguela transform-rifted margin segment to the oblique-rifted South Kwanza and orthogonal-rifted North Kwanza margin segments. The spatial variation in the intensity of post-rift uplift is demonstrated by the study of a set of geomorphic markers detected in the post-rift succession of the coastal Benguela and Kwanza Basins: Upper Cretaceous to Cenozoic uplifted palaeodeltas, erosional unconformities, palaeovalleys, Quaternary marine terraces and perched Gilbert deltas. The onshore Benguela transform margin has a distinctive, mainly progradational stratigraphic architecture with long-term sedimentary gaps and high-elevation marine terraces resulting from moderate Upper Cretaceous–Cenozoic to major Quaternary uplifting (i.e. 775–1775 mm/ky or m/Ma). By contrast, repeated synchronous episodes of minor Cenozoic to Quaternary uplift occurred along the orthogonal-rifted North Kwanza segment with its Cenozoic aggradational architecture, short-term sedimentary gaps and low-elevation Pleistocene terraces. Margin style likewise governs spatial variations in the volume of offshore sediment dispersed in the associated deep-sea fans. Along the low-lying North Kwanza margin, sedimentation of the broad Cenozoic to Pleistocene Kwanza submarine fan was probably governed by the width of the Kwanza interior palaeodrainage basin combined with the wet tropical Neogene climate. Along the high-rising Benguela margin, the small size of the Benguela deep-sea fan is related to the interplay between moderate continental sediment dispersal from long-lived small catchments and a warm, very arid Neogene climate. However, the driving forces behind the epeirogenic post-rift uplift of the Angola coastal bulge remain a matter of speculation.  相似文献   

http://www.sciencedirect.com/science/article/pii/S1674987110000319   总被引：1，自引：1，他引：0  

Jiasheng Zhang  Xinjian Shan  Xiongnan Huang 《地学前缘(英文版)》2011,2(1):1-15

The 3-D geometry of the seismicity in Hindu Kush–Pamir–western China region has been defined by seismic records for 1975–1999 from the National Earthquake Information Center, the U.S. Geological Survey, and over 16,000 relocated earthquakes since 1975 recorded by the Xinjiang seismic network of China. The results show that most Ms ≥ 5.0 hypocenters in the area are confined to a major intracontinental seismic shear zone (MSSZ). The MSSZ, which dips southwards in Pamir has a north-dipping counterpart in the Hindu Kush to the west; the two tectonic realms are separated by the sinistral Chaman transform fault of the India–Asia collisional zone. We demonstrate that the MSSZ constitutes the upper boundary of a south-dipping, actively subducting Pamir continental plate. Three seismic concentrations are recognized just above the Pamir MSSZ at depths between 45–65 km, 95–120 km, and 180–220 km, suggesting different structural relationships where each occurs. Results from focal mechanism solutions in all three seismological concentrations show orientations of the principal maximum stress to be nearly horizontal in an NNW–SSE direction. The south-dipping Pamir subduction slab is wedge-shaped with a wide upper top and a narrow deeper bottom; the slab has a gentle angle of dip in the upper part and steeper dips in the lower part below an elbow depth of ca. 80–120 km. Most of the deformation related to the earthquakes occurs within the hanging wall of the subducting Pamir slab. Published geologic data and repeated GPS measurements in the Pamir document a broad supra-subduction, upper crustal zone of evolving antithetic (i.e. north-dipping) back-thrusts that contribute to north-south crustal shortening and are responsible for exhumation of some ultrahigh-pressure rocks formed during earlier Tethyan plate convergence. An alternating occurrence in activity of Pamir and Chaman seismic zones indicates that there is interaction between strike-slip movement of the Chaman transform fault system and deep-subduction of the Pamir earthquake zone. Pamir subduction-related seismicity becomes shallower in depth with increasing distance east of the transform fault. Therefore, sinistral movement of the Chaman transform fault appears to be influencing continental deep-subduction in the Pamir region and may provide an explanation for the unusual south-dipping geometry of the intracontinental Pamir plate.  相似文献   

The High Resolution Chirp Transform Spectrometer for the Sofia-Great Instrument   总被引：1，自引：0，他引：1  

G. Villanueva  P. Hartogh 《Experimental Astronomy》2004,18(1-3):77-91

In this paper, we present the design of a high resolution Chirp Transform Spectrometer (CTS) which is part of the GREAT (German REceiver for Astronomy at Terahertz frequencies) instrument onboard SOFIA, the Stratospheric Observatory For Infrared Astronomy. The new spectrometer will provide unique spectral resolving power and linearity response, since the analog Fourier transform performed by the CTS spectrometer was improved through a new design, that we call “Adaptive Digital Chirp Processor (ADCP)”. The principle behind the ADCP consists on digitally generating the dispersive signal which adapts to the compressor dispersive properties, achieving maximum spectral resolution and higher dynamic range. Excellent test results have been obtained such as a white noise dynamic range of 30 dB, and a spectral resolution (FWHM) of 41.68 kHz which would mean if analyzing signals with the high frequency band receiver on the GREAT instrument (4.7 THz) a spectral resolving power (λ/Δ λ) higher than 10⁸.  相似文献   

应用不变特征获取均匀控制点的遥感影像配准算法   总被引：1，自引：0，他引：1  

倪希亮  丁琳  江涛  胡顺石 《测绘科学》2011,36(2):70-72

本文针对大幅影像配准时计算量大、配准点分布严重不均匀以及错配率高等问题进行了研究,提出一种可保持配准点均匀分布的快速配准算法.首先对基准影像和待配准影像进行分块提取SIFT特征算子,然后局部自适应地对影像块中的匹配点进行几何约束,从局部选取最优匹配点以达到提高图像匹配准确率的目标.通过对大量不同类型的影像进行配准实验,...  相似文献   

Application of Fractional Fourier Transform in seismic data denoising     

ZHANG Zongbao  LIU Cai 《世界地质(英文版)》2014,17(2):110-114

Data processing is a basic and crucial factor in seismic exploration,which can influence the effect of subsequent processing directly． Thus the selection of appropriate method for data processing is one of the most important tasks throughout the work． By simulating,the authors analyze and compare Fractional Fourier Trans- form (FＲFT) and Wigner-Ville distribution (WVD),then summarize the similarities and advantages and dis- advantages of the two methods． The results reveal that FＲFT is more effective and suitable for application in seismic exploration than WVD．  相似文献