海洋天然气水合物勘探地震处理的最小平方反滤波设计及其应用     

杨胜雄  符溪  吴亚东  文鹏飞 《海洋学报》2004,26(3):75-81

地震勘探的BSR识别技术是发现海洋天然气水合物的最经济、快捷、方便、有效的方法.在地震处理识别上,对子波的精确处理是水合物地震资料处理中最关键的一个环节,采用最小平方误差准则,即利用实际输出与期望输出的误差平方和为最小的条件,来确定反滤波因子,因此又称为最小平方子波整形.在地震处理程序中引入三种期望输出,即俞氏子波、雷克子波、Buttworth子波,对子波零相位化有较好的效果.根据上面的原理,我们开发了一套最小平方反滤波地震处理软件,对天然气水合物地震勘探资料进行试处理的结果表明,该软件在提高分辨率的同时保持了较高的信噪比.  相似文献   

Ill-conditioning and pre-whitening in seismic deconvolution     

R. J. O'Dowd 《Geophysical Journal International》1990,101(2):489-491

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Integrated 3D density modelling and segmentation of the Dead Sea Transform     

H.-J. Götze  R. El-Kelani  S. Schmidt  M. Rybakov  M. Hassouneh  H.-J. Förster  J. Ebbing  DESERT Group 《International Journal of Earth Sciences》2007,96(2):289-302

A 3D interpretation of the newly compiled Bouguer anomaly in the area of the “Dead Sea Rift” is presented. A high-resolution 3D model constrained with the seismic results reveals the crustal thickness and density distribution beneath the Arava/Araba Valley (AV), the region between the Dead Sea and the Gulf of Aqaba/Elat. The Bouguer anomalies along the axial portion of the AV, as deduced from the modelling results, are mainly caused by deep-seated sedimentary basins (D > 10 km). An inferred zone of intrusion coincides with the maximum gravity anomaly on the eastern flank of the AV. The intrusion is displaced at different sectors along the NNW–SSE direction. The zone of maximum crustal thinning (depth 30 km) is attained in the western sector at the Mediterranean. The southeastern plateau, on the other hand, shows by far the largest crustal thickness of the region (38–42 km). Linked to the left lateral movement of approx. 105 km at the boundary between the African and Arabian plate, and constrained with recent seismic data, a small asymmetric topography of the Moho beneath the Dead Sea Transform (DST) was modelled. The thickness and density of the crust suggest that the AV is underlain by continental crust. The deep basins, the relatively large intrusion and the asymmetric topography of the Moho lead to the conclusion that a small-scale asthenospheric upwelling could be responsible for the thinning of the crust and subsequent creation of the Dead Sea basin during the left lateral movement. A clear segmentation along the strike of the DST was obtained by curvature analysis: the northern part in the neighbourhood of the Dead Sea is characterised by high curvature of the residual gravity field. Flexural rigidity calculations result in very low values of effective elastic lithospheric thickness (t _e < 5 km). This points to decoupling of crust in the Dead Sea area. In the central, AV the curvature is less pronounced and t _e increases to approximately 10 km. Curvature is high again in the southernmost part near the Aqaba region. Solutions of Euler deconvolution were visualised together with modelled density bodies and fit very well into the density model structures. An erratum to this article can be found at  相似文献   

Receiver Functions from Autoregressive Deconvolution   总被引：4，自引：0，他引：4  

Qingju Wu  Yonghua Li  Ruiqing Zhang  Rongsheng Zeng 《Pure and Applied Geophysics》2007,164(11):2175-2192

Summary Receiver functions can be estimated by minimizing the square errors of Wiener filter in time-domain or spectrum division in frequency domain. To avoid the direct calculation of auto-correlation and cross-correlation coefficients in Toeplitz equation or of auto-spectrum and cross-spectrum in spectrum division equation as well as empirically choosing a damping parameter, autoregressive deconvolution is presented to isolate receiver function from three-component teleseismic P waveforms. The vertical component of teleseismic P waveform is modeled by an autoregressive model, which can be forward and backward, predicted respectively. The optimum length of the autoregressive model is determined by the Akaike criterion. By minimizing the square errors of forward and backward predicting filters, autoregressive filter coefficients can be recursively solved, and receiver function is also estimated in the similar procedure. Both synthetic and real data tests show that autoregressive deconvolution is an effective method to isolate receiver function from teleseismic P waveforms in time-domain.  相似文献   

图像小波域维纳滤波去噪算法的改进     

严勇  陈钟荣 《南京气象学院学报》2005,28(5):685-689

介绍了小波变换和维纳滤波相结合的图像小波域维纳滤波去噪算法，在分析该算法最小均方误差期望的基础上提出一种改进算法。指出在进行维纳滤波之前，阈值化处理可以有效提高维纳滤波的性能。用标准测试图像的处理结果来比较改进前后两种算法的效果。  相似文献   

Stable inverse deconvolution of magnetic data     

Fabio Caratori Tontini 《Geophysical Journal International》2005,162(3):725-735

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On the determination of magnetic grain-size distributions of superparamagnetic particle ensembles using the frequency dependence of susceptibility at different temperatures   总被引：1，自引：0，他引：1  

Valera P. Shcherbakov  Karl Fabian 《Geophysical Journal International》2005,162(3):736-746

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维纳滤波技术及其在新疆地区重力场划分中的应用     

蒋甫玉  孟令顺  张凤旭  贾真  刘丹 《吉林大学学报(地球科学版)》2007,37(5):1016-1022

基于维纳滤波原理,应用多层格林等效层模型模拟实测重力场的径向对数功率谱,采用改进的格拉姆-施密特正交化方法计算功率谱密度函数,确保了数值的稳定性,得到了较为满意的结果。通过理论模型实验,证实了利用维纳滤波方法提取深部场时可以保证低频成分不衰减的功能,能够较为精确地提取区域异常,从而实现频率域中位场的分离。运用维纳滤波方法对新疆地区布格重力异常进行了分离处理,获得了基于最佳滤波原理计算的新疆地区区域重力异常,并根据新疆地区布格异常和区域场特征,划分了9条深大断裂和5个一级构造单元。  相似文献   

基于局部维纳滤波的交通图像去雾霾算法   总被引：1，自引：0，他引：1  

肖杰  李同亮  翟东海 《成都信息工程学院学报》2014,(6):567-573

为了提高雾霾天退化交通图像的色彩保真度和清晰度,基于局部维纳滤波并结合暗通道先验理论提出一种快速去雾霾算法。传统的基于暗通道先验理论的去雾霾算法对单一户外场景图像取得了不错的效果,但在处理较高分辨率交通图像时,需要消耗大量的计算和存储资源;同时,不能很好处理图像中的一些白色区域,会导致该区域色彩失真。针对这两个问题展开研究:首先,基于局部维纳滤波并结合暗通道先验原则优化大气散射光,进而得到细化的透射率;其次,通过动态调节参数的大小以适应天空等明亮区域地去雾霾处理;最后,将所提算法用于实例验证,结果表明算法不但可以保证交通图像白色区域的色彩不失真,而且去雾霾效率提高4~25倍。  相似文献   

地面磁梯度测量在勘查地下污水管道中的应用     

任秀艳  杜晓娟  孙瑞雪  逄硕  王江  高超 《世界地质(英文版)》2014,(3)

利用在辽宁某地区实测的垂直磁梯度数据,采用欧拉反褶积方法对地下异常情况进行处理和解释。正演研究表明,理论计算获得的磁梯度比实测磁总场的灵敏度高,结合磁梯度数据和欧拉反演方法可以进行较为复杂地形的解释。通过将计算获得的磁梯度异常与实测磁梯度异常对比,后者对地质体的分辨率更高。对地面垂直磁梯度数据进行反演,结果表明：该方法能够准确地确定地下污水管道的边界和埋深。  相似文献