BC87数据的电场和磁场畸变分解。

A. Chave, A. Jones
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引用次数: 44

摘要

BC87大地电磁数据由于各种尺度的三维结构而表现出扭曲,从非常局部到区域。以前的工作表明,这些扭曲有时可以(但并不总是)用电场电场扭曲模型来描述,因此可以使用张量分解方法来消除。这项工作扩展了分析,包括磁场的电流畸变,并显示了它对许多BC87点的重要性。然而,即使是电场和磁场相结合的电流畸变方法也无法在相当多的研究地点实现。这种现象在短于10秒的周期内普遍存在,这表明存在局部三维感应效应,但在较长周期内模型的不足可能表明模型假设的失败,特别是对区域电场在扭曲体上均匀且与观测点相当的要求。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Electric and Magnetic Field Galvanic Distortion Decomposition of BC87 Data.
The BC87 magnetotelluric data exhibit distortions due to three-dimensional structures at all scale sizes, from very local to regional. Previous work has shown that these distortions can sometimes, but not always, be described by an electric field galvanic distortion model, and hence can be removed using a tensor decomposition approach. This work extends the analysis to include galvanic distortion of the magnetic field, and shows its importance for many of the BC87 sites. However, even a combined electric and magnetic field galvanic distortion approach fails for quite a few of the sites studied. This is pervasive for periods shorter than 10 s, suggesting local 3D inductive effects, but model inadequacy at longer periods may indicate a breakdown of the model assumptions, particularly the requirement that the regional electric field be both uniform across the distorting body and comparable to that at the observation point.
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