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The linear theory of antisymmetric ducted gravity waves supported by mesospheric thermal duct is presented, propagation and evolution of gravity wave packets in thermal duct is also simulated by using a nonlinear two-dimensional model. Numerical results show that lower atmospheric wave disturbance can penetrate into the duct area and be trapped.

给出了重力波在中层大气温度波导中的反对称形式导制传播的线性理论模型,并采用二维非线性的数值模型对重力波波包在中层大气温度波导中的传播和演变过程进行了模拟研究。

It is popular to identify the fault and inverse the parameters of the fault with Bouguer gravity anomaly in gravity exploration.

在重力勘探中,一般都要利用布格重力异常来识别断层和反演断层的参数。

There are intimate connection between the Bouguer gravity anomaly and the Moho depth, so it is one of main methods to inverse the Moho depth according to gravity anomaly.

布格重力异常与莫霍面深度之间具有紧密的联系,利用重力异常反演莫霍面深度成是研究莫霍面深度和编制莫霍面深度图的主要手段之一。

In this paper, we put forward a 2.5D model based on the hexahedron and developed an inversion method of constraint gravity-vertical fault. The inversion result is better than that the 2D model through the model tests. Based on this model, we quantitatively interpreted the Bouguer gravity anomaly of the Sierra Nevada Region in the USA.

本文从六面体模型出发,将二度体模型修改为似二度体模型,建立了一个带约束的重力-垂直断层反演模型,经过理论模型试验,证明效果要优于二度体模型的反演结果,在此基础上对美国内华达州的圣安德烈斯地区的布格重力异常资料做了定量解释。

At the end the test of ground gravity solution from simulated satellite data and down continuation of airborne gravimetry are conducted.

提出并建立了球面小波正则化方法,建立了不适定问题的渐近逼近解,利用这种方法进行了模拟卫星数据反解地面重力位试验以及航空重力测量数据向下延拓试验。

In this paper, we put forward a 2.5D model based on the hexahedron and an inversion method of constraint gravity-vertical fault.

本文从六面体模型出发,将二度体模型修改为似二度体模型,建立了一个带约束的重力-垂直断层反演模型,经过理论模型试验证明效果要优于二度体模型的反演结果,在此基础上对美国内华达州的圣安德烈斯地区的布格重力异常资料做了定量解释。

The discussion is concentrated on such important aspects of gravity methods as: the processing and inverse methods of gravity data, the theory and application of the isostasy, and the application of the satellitic gravity data for the deep structure interpretation.

对于重力方法的几个重要内容:重力资料的数据处理和反演方法,均衡理论和应用,卫星重力资料在深部构造解释中的应用等几个方面展开了讨论。

Based on the relationship between the gravity anomaly and mass deficiency of the ocean, the 2.5¢′2.5¢ bathymetry model in the south sea of China is inversed using multi-satellite altimeter data and geophysical data. In the study, the FFT technique has been put in practice, and the effect of proportion has been considered.

深入讨论了重力异常与海深之间的关系;在考虑地壳均衡补偿效应影响的基础上,推导了由重力异常利用 FFT 技术计算海深的模型;然后利用推导的模型联合测高卫星数据和海洋重力资料反演了中国南海2.5¢′2.5¢海底地形。

In order to locate mined-out areas in gold mines and place a curb on its hidden hazard, through laying out two high precision gravity survey sections of the 1∶100 scale in the research area, with Canadian Scintrex Corporation′s CG-5AutoGrav gravimeter, the gravity anomaly data are measured by the high precision gravity survey method for the first time, and the inversion is made by the Euler deconvolution method to determine the collapse of the mined-out region and the stable sector.

为了确定金矿采空区的位置,对其隐患进行治理,首次应用高精度重力方法。在研究区布设了两条比例尺为1∶100的高精度重力测量剖面,使用加拿大Scintrex公司的CG-5AutoGrav型重力仪,测取重力异常数据,并采用欧拉反褶积方法实施反演解释,确定了采空塌陷区域及稳定地段。

Many new methods, such as reduction of gravity data to a horizontal plane, wavelet analysis, higher order statistics, joint inversion and intera...

山区重力资料曲化平,小波分析及高阶统计量等现代信号处理方法,重震、重磁、电震的联合反演与交互反演,三维可视化反演,BP人工神经网络方法等在综合地球物理处理解释中得到广泛应用。

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