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A wavenumber-domain iterative approach for apparent density mapping of an undulant layer and its application in central South China

机译:非胸部层的表观密度映射的波数域迭代方法及其在中国中部的应用

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摘要

Apparent density mapping is a technique to invert the gravity anomaly for obtaining the density distribution in the subsurface layer. The conventional approach for apparent density mapping usually assumes that the top and bottom interfaces of the layer are flat and horizontal, which is not often the case in the real world. We have developed a wavenumber-domain iterative approach for mapping a density distribution of the undulant layer, whose top and bottom interfaces could be a variable relief. The wavenumber-domain approach requires that the observational surface of the gravity data is flat and horizontal. The wavenumber-domain equations for forward calculation of the gravity anomaly due to the undulant layer and its inversion are presented. A damping factor is adopted in the inversion equation for suppressing high-frequency noise in the data and stabilizing the mapping. We use an iterative algorithm for mapping to minimize the difference between the observed and calculated gravity anomalies and to optimize the density values within the layer. The presented approach is simple, fast, stable, and easy to operate. A test on the synthetic data and the real data from the Xuefengshan tectonic zone in central South China verified the feasibility of our approach with higher accuracy than the conventional wavenumber-domain mapping approaches and higher efficiency than the conventional space-domain mapping approach.
机译:表观密度映射是反转重力异常以获得地下层中的密度分布的技术。用于表观密度映射的传统方法通常假设该层的顶部和底部界面是平坦的,水平的,这在现实世界中通常是不常的。我们开发了一种用于映射未浮动层的密度分布的波数域迭代方法,其顶部和底部接口可能是可变的浮雕。波数 - 域方法要求重力数据的观察表面是平坦的水平的。提出了由于出于未浮动层和反转而导致重力异常的波数域方程。在反演方程中采用阻尼因子,以抑制数据中的高频噪声并稳定映射。我们使用迭代算法来映射,以最小化观察和计算的重力异常之间的差异,并优化层内的密度值。提出的方法简单,快速,稳定,操作易于操作。南方中部雪峰山构造区的合成数据和实际数据的测试验证了我们的方法的可行性,比传统的波数域映射方法和更高的效率高于传统的空间域映射方法。

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