Reflection and transmission of elastic waves at a loosely bonded interface between an elastic solid and liquid-saturated porous solid     

A. K. Vashisth  M. D. Sharma  M. L. Gogna 《Geophysical Journal International》1991,105(3):601-617

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浅层地震反射波资料处理在微型计算机上的实现     

孙渊  王玉贵 《地球科学与环境学报》1988,(4)

本文对浅层反射资料的常规处理在微机(Dual 68000。和IBM PC/XT)上的实现做一简单介绍.由于方法原理众所周知,因此只就处理模块的功能和特点以及实际应用作一讨论,并对目前我教研室浅层地震资料处理的软件开发工作和设想作一介绍.  相似文献   

Frozen Hydrocarbon Particles as a Luminescent Dust Component of Nebular Matter     

I. A. Simonia 《Astrophysics》2005,48(3):374-380

This paper is a continued examination of luminescence of cosmic dust, in particular the dust in reflecting nebulae. A model of frozen hydrocarbon particles in the form of a nucleus with a polycrystalline mantle is proposed. The basic properties of these particles, as well as the technique for obtaining spectra of the nebula CED 201 on the 2 meter TLS telescope with a Naismith focus spectrograph, are described. Part of the detected unknown emission in the spectrum of CED 201 is identified as photoluminescence of frozen hydrocarbon particles that form part of the dust component of the nebular matter.__________Translated from Astrofizika, Vol. 48, No. 3, pp. 445–453 (August 2005).  相似文献   

双参数展开CRP叠加和速度分析方法研究   总被引：1，自引：0，他引：1       下载免费PDF全文

周青春  刘怀山  Kondrashkov V V  李国都  林依华 《地球物理学报》2009,52(7):1881-1890

椭圆展开共反射点(CRP)方法可以获得比常规倾角时差校正(DMO)方法更近似的零偏移距时间剖面和相应CRP速度场.大量研究和实践证实,在非均质性较弱的地区,该方法取得的成果显著.但由于该方法没有考虑速度的横向变化和转换波等情况,当地下介质存在较强非均质性时,该方法不再准确,需要引进反映速度横向变化的双参数(上行波与下行波的平均速度和速度比)进行改进.本文详细推导了引入双参数后的叠加和速度分析算法,并通过数值模型和地震资料处理证实,修正后的算法可以更好地解决地质复杂地区速度建模和叠加成像问题.  相似文献   

等效偏移距偏移方法在声波反射成像测井中的应用研究(英文)   总被引：2，自引：1，他引：1  

张铁轩  陶果  李君君  王兵  王华 《应用地球物理》2009,6(4):303-310

声波反射成像测井能够获得井眼周围构造的重要信息,然而,由于接收到的反射波信号远小于井眼模式波、信噪比较低,且每次发射只有8道接收,因此应用常规的偏移成像处理方法成像效果不好。本文应用一种基于散射理论的等效偏移距偏移方法,对声波反射成像测井模拟数据及现场数据进行偏移处珲。结果表明,与常规叠后深度偏移方法相比,等效偏移距方法可以有效提高覆盖次数,对于低信噪比的声波反射测井资料可以获得较好的井旁构造成像效果。  相似文献   

A Formal Theory for Vortex Rossby Waves and Vortex Evolution     

James C. McWilliams  Lee P. Graves  Michael T. Montgomery 《地球物理与天体物理流体动力学》2013,107(4):275-309

A formal theory is presented for the balanced evolution of a small-amplitude, small-scale wave field in the presence of an axisymmetric vortex initially in gradient-wind balance and the accompanying changes induced in the vortex by the azimuthally averaged wave fluxes. The theory is a multi-parameter, asymptotic perturbation expansion for the conservative, rotating, f-plane, shallow-water equations. It extends previous work on Rossby-wave dynamics in vortices and more generally provides a new perspective on wave/mean-flow interaction in finite Rossby-number regimes. Some illustrative solutions are presented for a perturbed vortex undergoing axisymmetrization.  相似文献   

Seismic velocity structure of a large mafic intrusion in the crust of central Denmark from project ESTRID   总被引：1，自引：1，他引：0  

H. Thybo  A. Sandrin  L. Nielsen  H. Lykke-Andersen  G.R. Keller 《Tectonophysics》2006,420(1-2):105

The origin of regional sedimentary basins is being investigated by the ESTRID project (Explosion Seismic Transects around a Rift In Denmark). This project investigates the mechanisms of the formation of wide, regional basins and their interrelation to previous rifting processes in the Danish–Norwegian Basin in the North Sea region. In May 2004 a 143 km long refraction seismic profile was acquired along the strike direction of a suspected major mafic intrusion in the crust in central Denmark. The data confirms the presence of a body with high seismic velocity (> 6.5 km/s) extending from a depth of  10–12 km depth into the lower crust. There is a remarkable Moho relief between 27 and 34 km depth along this new along-strike profile as based on ray-tracing modelling of PmP reflections. The lack of PmP reflections at a zone of very high velocity in the lowest crust (7.3–7.5 km/s) suggests a possible location of a feeder channel to the batholith. The presence of volcanic rocks of Carboniferous–Permian age above the intrusion (mafic batholith) suggests a similar age of the intrusion. An older obliquely crossing profile and two new fan profiles deployed perpendicular to the main ESTRID profile, show that the batholith is about 30–40 km wide. The existence of this large mafic batholith supports the hypothesis that the origin of the Danish–Norwegian Basin is related to cooling and contraction after intrusion of large amounts of mafic melts into the crust during the late Carboniferous and early Permian. The data and interpretations from project ESTRID will form the basis for subsidence modelling. Tentatively, we interpret the formation of the Danish–Norwegian Basin as a thermal subsidence basin, which developed after widespread rifting of the region.  相似文献   

The orbital period and negative superhumps of the nova-like cataclysmic variable V378 Pegasi     

F.A. Ringwald  Kenia VelascoJonathan J. Roveto  Michelle E. Meyers 《New Astronomy》2012,17(4):433-437

A radial velocity study is presented of the cataclysmic variable V378 Pegasi (PG 2337 + 300). It is found to have an orbital period of 0.13858 ± 0.00004 d (3.32592 ± 0.00096 h). Its spectrum and long-term light curve suggest that V378 Peg is a nova-like variable, with no outbursts. We use the approximate distance and position in the Galaxy of V378 Peg to estimate E(B − V) = 0.095, and use near-infrared magnitudes to calculate a distance of 680 ± 90 pc and M_V = 4.68 ± 0.70, consistent with V378 Peg being a nova-like. Time-resolved photometry taken between 2001 and 2009 reveals a period of 0.1346 ± 0.0004 d (3.23 ± 0.01 h). We identify this photometric variability to be negative superhumps, from a precessing, tilted accretion disk. Our repeated measurements of the photometric period of V378 Peg are consistent with this period having been stable between 2001 and 2009, with its negative superhumps showing coherence over as many as hundreds or even thousands of cycles.  相似文献   

日本“311”海啸对江苏北部沿海影响分析     

袁春光  王义刚  黄惠明  蔡辉  陈橙 《海洋工程》2013,31(6):68-75

北京时间2011年3月11日13时46分日本东北部发生里氏9.0级强烈地震,江苏北部的灌河口潮位站正好记录下海啸期间的潮位资料。由于以往对海啸波动的过滤提取方法不统一,而且人为因素影响较大,误差积累影响了后续科研工作的进行。提出综合利用小波能谱、功率谱和滤波分析等方法结合海啸识别结果来提取海啸波的方法,并且成功提取出灌河口站海啸波的周期范围、影响时间和最大波峰。同时采用COMCOT海啸数学模型,讨论了江苏沿海海啸波传播方式,解释了灌河口潮位站海啸波最大波峰未出现在第一波的原因,是因为江苏北部山东半岛特殊的地形使得在黄海传播的海啸波发生反射,与之前的波动产生叠加效果导致的。分析结果表明:江苏沿海由于海啸直接引起的海啸波不高,但是海啸波叠加之后,最大波高却是之前的2倍,因此在海啸预报中应该全面考虑地理位置特点,分析海啸波运动的反射叠加等特征,从而提高预报质量。  相似文献   

梳状防波堤上波浪反射     

傅朝方  朱大同 《海洋工程》2013,31(4):37-41

对梳状沉箱防波堤的波浪反射特征进行研究。在对梳状沉箱防波堤非线性消耗波能机理分析基础上,采用阻抗分析方法,导出一组所有参数都是事先知道的、完全封闭的波反射系数公式。  相似文献