傅立叶相位分析导风技术中的频谱分析   总被引：1，自引：0，他引：1  

许建明  王振会 《气象科学》2005,25(5):499-504

本文介绍了应用于傅立叶相位分析导风技术中的DFT变换理论,并模拟分析DFT计算中的频谱分离和混叠两种现象及其对导风的影响。结论认为,傅立叶导风技术不需要计算所有谐波的相位,只要计算分离区或混叠区之前的低次谐波的相位,这些低次谐波的相位速度与真实速度一致,且与谐波振幅和初相位的取值无关,可用于风速计算。  相似文献   

基于中轴变换算法的室内外一体化导航路网自动生成方法     

武恩超  张恒才  吴升 《地球信息科学学报》2018,20(6):730-737

室内外一体化导航路网的快速生成与更新对面向行人的跨场景导航具有重要意义。当前研究主要关注单一场景下的导航路网构建,对于跨室内外场景的导航路网自动生成研究较少。本文基于对偶图思想与二维平面多边形中轴变换（Medial Axis Transform）算法,提出一种室内外一体化导航路网自动生成方法,并以某建筑CAD平面图及周边路网环境为基础数据进行了实例研究。结果表明：该方法能够根据原始数据的几何、拓扑、语义信息自动构建导航路网,并支持室内外跨场景的最短路径查询,在最短路径查询效率上较传统分场景寻路模型整体提升10.18%;相较单一场景下的导航路网,一体化导航路网可结合语义信息将室内及室外导航路网有机统一起来,解决跨场景寻求最优路径的问题,为最优路径规划的相关研究提供了新的思路。  相似文献   

南海东北部陆缘地壳结构特征及下地壳高速层成因          下载免费PDF全文

李海龙  吴招才  许明炬 《海洋学研究》2019,37(2):44-56

南海东北部陆缘构造演化信息丰富,对于理解南海的演化过程至关重要。本文收集了南海东北部的深反射地震和海底广角地震成果剖面,提取地壳和下地壳高速层的厚度结果,并结合水深、重磁异常和岩石圈的流变学等地质地球物理资料,对南海东北部的地壳减薄特征、吕宋-琉球转换板块边界的性质和下地壳高速层的分布及成因进行了分析和讨论。南海东北部的地壳减薄在横向和垂向上都存在不均匀性,以下地壳减薄为主,在台西南盆地存在极端减薄地壳;南海北缘的白云凹陷、西沙海槽和西缘的中建南盆地也存在类似的极端减薄地壳,且都与刚性地块共轭或邻近,推测刚性地块的存在导致地壳初始破裂时下地壳流动和地幔上隆是局部出现地壳极端减薄的主要原因。吕宋-琉球转换板块边界两侧在海底地形、新生代反射和重磁异常等方面均存在差异,与中生代岛弧引起的高磁异常大角度相交,其可能是中生代古特提斯构造域向太平洋构造域转换的边界断裂。下地壳高速层在南海东北部广泛发育,结合其分布特征和波速比V_p/V_s的分布区间,认为其是多期次岩浆底侵形成的铁镁质基性岩。  相似文献   

Seismic stratigraphy and structure of the Northland Plateau and the development of the Vening Meinesz transform margin,SW Pacific Ocean     

R. H. Herzer  B. W. Davy  N. Mortimer  P. G. Quilty  G. C. H. Chaproniere  C. M. Jones  A. J. Crawford  C. J. Hollis 《Marine Geophysical Researches》2009,30(1):21-60

The Northland Plateau and the Vening Meinesz “Fracture” Zone (VMFZ), separating southwest Pacific backarc basins from New Zealand Mesozoic crust, are investigated with new data. The 12–16 km thick Plateau comprises a volcanic outer plateau and an inner plateau sedimentary basin. The outer plateau has a positive magnetic anomaly like that of the Three Kings Ridge. A rift margin was found between the Three Kings Ridge and the South Fiji Basin. Beneath the inner plateau basin, is a thin body interpreted as allochthon and parautochthon, which probably includes basalt. The basin appears to have been created by Early Miocene mainly transtensive faulting, which closely followed obduction of the allochthon and was coeval with arc volcanism. VMFZ faulting was eventually concentrated along the edge of the continental shelf and upper slope. Consequently arc volcanoes in a chain dividing the inner and outer plateau are undeformed whereas volcanoes, in various stages of burial, within the basin and along the base of the upper slope are generally faulted. Deformed and flat-lying Lower Miocene volcanogenic sedimentary rocks are intimately associated with the volcanoes and the top of the allochthon; Middle Miocene to Recent units are, respectively, mildly deformed to flat-lying, calcareous and turbiditic. Many parts of the inner plateau basin were at or above sea level in the Early Miocene, apparently as isolated highs that later subsided differentially to 500–2,000 m below sea level. A mild, Middle Miocene compressive phase might correlate with events of the Reinga and Wanganella ridges to the west. Our results agree with both arc collision and arc unzipping regional kinematic models. We present a continental margin model that begins at the end of the obduction phase. Eastward rifting of the Norfolk Basin, orthogonal to the strike of the Norfolk and Three Kings ridges, caused the Northland Plateau to tear obliquely from the Reinga Ridge portion of the margin, initiating the inner plateau basin and the Cavalli core complex. Subsequent N115° extension and spreading parallel with the Cook Fracture Zone completed the southeastward translation of the Three Kings Ridge and Northland Plateau and further opened the inner plateau basin, leaving a complex dextral transform volcanic margin.  相似文献   

Rift–shear architecture and tectonic development of the Ghana margin deduced from multichannel seismic reflection and potential field data     

A.A. Antobreh  J.I. Faleide  F. Tsikalas  S. Planke 《Marine and Petroleum Geology》2009

The Ghana margin displays one of the best-known transform margins. Studies of the margin have provided the framework for a number of conceptual models aimed at understanding transform margin development worldwide. However, the deep structure of the margin is poorly known as knowledge is based only on wide-angle refraction measurements obtained from two separate localities on the margin. Consequently, complexities in the rift–shear margin architecture have been overlooked by current interpretations of margin development. Based on combined analysis of a detailed grid of ∼2710 km multichannel (MCS) lines and potential field data, we provide new insights into the structural architecture and tectonic development of the Ghana margin. In particular, we outline the deep structure of the entire margin using a series of 2D gravity modelled transects constrained by MCS and published wide-angle data. Our study reveals more complex rift–shear margin architecture than previously envisaged. We demonstrate that the main transform boundary representing the continental extension of the Romanche Fracture Zone, is actually composed of two distinct margin segments, i.e., the ENE–WSW trending sheared margin segment of the Cote d’Ivoire-Ghana Ridge and the NE–SW trending rift-influenced sheared margin segment of the Ghana Platform. These segments evolved under varying stress regimes, and during different time intervals. West of the transform margin, divergent rifting during the Early Cretaceous initiated the development of the Deep Ivorian Basin, essentially, as a single major pull-apart structure. However, east of the shear zone, oblique rifting resulted in the development of the Eastern Ghana Slope Basin as a composite of at least two coalescing pull-apart basins displaced along strike-slip faults. Our structural interpretation of the transform boundary geometry shows that the ridge and platform margin segments were each subjected to separate thermal influences from two different migrating spreading centres. Tectonic uplift of the ridge began through transpression during mid-Albian time following a change in relative direction of plate motion from NE–SW to ENE–WSW. However, the ridge uplift was amplified by thermal heating from a previously undocumented spreading centre whose progressive westward migration along the ridge followed closely after the Albian transpressional phase. The structural architecture of the Ghana margin resulted from a combination of factors, notably, pre-existing basement structure, plate boundary geometry, the relative direction of plate motion and thermal heating.  相似文献   

超导重力仪观测数据分析与信号检测          下载免费PDF全文

邢喆  杨柳  李鹏 《海洋测绘》2008,28(2):40-43

探测时间序列中隐藏的周期信号是超导重力仪观测数据分析的目标之一,进行超导重力仪观测数据中隐含信号的检测,最常用的方法是快速傅里叶变换(Fast Fourier Transform ation,FFT)。首先对快速傅里叶变换的原理加以介绍,然后,结合1998年加拿大站全年的超导重力观测数据实例,详细讨论了用快速傅里叶变换进行谱分析的步骤,最后对数据结果进行了分析。  相似文献   

加权抛物Radon变换叠前地震数据重建   总被引：16，自引：6，他引：10       下载免费PDF全文

王维红  裴江云  张剑锋 《地球物理学报》2007,50(3):851-859

基于部分动校正（NMO）后反射同相轴在CMP道集上的抛物线走时近似,给出了加权抛物Radon变换叠前地震数据重建方法（WPRT）. WPRT通过在迭代过程中引入变化着的权系数,拓展和改进了传统抛物Radon变换方法,使其可同时完成不规则采样的规则化和空道及近偏移距道重建,且有更高的计算效率. 文中给出了应用WPRT进行近偏移距和中偏移距的空地震道重建及数据规则化的算法实现. 理论模型和实际地震资料的地震数据重建结果显示了本文算法的优点.  相似文献   

三种变换在强震记录分析方面的研究     

连海宁  谢礼立 《华北地震科学》2007,25(3):28-33

在简要地介绍比较了傅立叶变换、小波变换、希尔伯特-黄变换理论的基础上,针对集集地震大量强震记录进行各种变换分析比较,以探求希尔伯特-黄变换在强震记录分析中应用的前景.通过对集集地震60条不同震中距和场地的强震纪录,分别作傅立叶频谱、希尔伯特-黄边际谱和能量密度谱分析,列表归纳对比显示希尔伯特-黄变换在强震记录处理中基本表现出和其他变换相同的趋势,并有其新特点,能体现出强地震动的瞬时特性,是对现有强震数据处理方法重要的补充.  相似文献   

结合多尺度几何分析和KICA的遥感图像变化检测     

吴一全  曹照清  陶飞翔 《遥感学报》2015,19(1):126-133

为了进一步提高基于独立分量分析ICA(Independent Component Analysis)的遥感图像变化检测精确度,更好地实现地表覆盖的动态监测,将多尺度几何分析和核独立分量分析KICA(Kernel Independent Component Analysis)相结合应用于遥感图像的地表覆盖变化检测。首先利用Contourlet变换、复Contourlet变换CCT(Complex Contourlet Transform)、非下采样Contourlet变换NSCT(Nonsubsampled Contourlet Transform)等多尺度几何分析对土地遥感图像进行多尺度分解;然后对分解后的数据进行核独立分量分析,通过核函数将数据映射到高维特征空间中,再在该空间中用ICA方法分离出互相独立的分量;最后将分离后的地表变化分量转化为图像分量,再采用最大类间方差法对变化图像进行分割,实现地表覆盖的变化检测。给出了本文方法和近年来提出的基于ICA、基于KICA、基于小波变换和ICA等变化检测方法的实验结果,并进行了分析和定量比较。实验结果表明,基于多尺度几何分析和KICA的变化检测方法能更好地分离出遥感图像的变化信息,其中基于NSCT和KICA方法的错判和漏检误差最小,且在边缘细节方面处理得更好,而基于Contourlet变换和KICA方法的检测效率相对较高。  相似文献   

一维HHT变换在探地雷达数据处理中的应用     

王超  沈斐敏 《工程地质学报》2015,23(2):328-334

探地雷达(GPR)噪声信号通常具有非稳态、非线性特征,为去除这些噪声提高GPR图像解译的准确性,对利用HHT方法去噪进行了研究。首先阐述HHT的基本理论,然后通过对探地雷达数值模拟信号中噪声的去除验证基于HHT方法的可行性,最后将该方法用于探地雷达隧道地质超前预报的数据处理中。通过研究表明:该方法可以用于探地雷达信号的去噪,通过Hilbert变换得到三特征参数图像与EMD分解后合成图像进行对比验证,从而达到提高GPR信号解译精度的目的。  相似文献