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Regional and Residual Gravity Anomaly Separation Using Singular Spectrum based Frequency Filtering Methods: A Case Study of Shallow Subsurface Modeling from Nagpur, India

机译:基于奇异频谱的频率滤波方法的区域和残留重力异常分离 - 以印度纳格尔的浅层地下建模为例

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摘要

We present here the application of a single and multichannel singular spectrum analysis (SSA)-based data filtering algorithm for regional and residual gravity field separation. Initially, the single-channel SSA method was tested on synthetic gravity profile data generated using Gravity and Magnetics Modelling System (GM-SYS), a gravity modeling software, for a sedimentary basin structure corrupted with Gaussian white noise and compared with the convnetional Fast Fourier transform (FFT)-based wave number (non-data adaptive) and discrete wavelet transform (semi-data-adaptive) filtering approaches. The comparative results show that the residual filtering of gravity data using the SSA method produces less/minimal artifacts compared to FFT-based wave number filtering and wavelet filtering methods. Following the synthetic examples, we further employed multichannel SSA-based frequency filtering on 2D gridded gravity data from Umred, Nagpur district, Maharashtra, India, to separate the residual anomaly for modelling the shallow subsurface structures. The modelled depth sections of two mutually perpendicular profiles suggest the presence of alluvium, Lameta, Kamthi and Barakar formations with varying thicknesses. The formations identified from the models show a clear match with the local geology and nearby borehole information. We suggest that the single and multichannel SSA based frequency filtering are robust approaches for separating regional and residual components from gravity anomalies.
机译:我们在这里介绍了一个和多通道奇异频谱分析(SSA)的数据过滤算法,用于区域和残留的重力场分离。最初,在使用重力和磁性建模系统(GM-SYS),重力建模软件的合成重力分布数据上测试单通道SSA方法,用于沉积盆地结构,与高斯白噪声损坏,与传道快速傅立叶相比基于变换(FFT)的波数(非数据自适应)和离散小波变换(半数据 - 自适应)过滤方法。比较结果表明,与基于FFT的波数滤波和小波滤波方法相比,使用SSA方法的重力数据的残余滤波产生较少/最小的伪像。在合成示例之后,我们进一步采用了来自Umred,Nagpur区,印度Maharashtra的2D包装重力数据的多声道SSA的频率滤波,以分离残留异常来建模浅层地下结构。两个相互垂直的曲线的模型深度部分表明存在具有不同厚度的加容量,拉米塔,Kamthi和Barakar形成。从模型中识别的地层显示出与当地地质和附近的钻孔信息的明显匹配。我们建议,基于单通道的SSA SSA的频率滤波是鲁棒方法,用于将区域和残留组分与重力异常分离。

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