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Quantitative interpretation of magnetic anomalies from bodies approximated by thick bed models in complex environments

机译:复杂环境中厚磁层模型近似的物体磁异常的定量解释

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摘要

Magnetic prospecting is a rapid and inexpensive geophysical tool and one of the most widely used methods for geophysical prospection throughout the world. However, the noise factors-such as inclined magnetization, complex geological structure of investigated areas, and uneven terrain relief-strongly obscure the interpretation of observed magnetic anomalies. The developed methodology of magnetic anomalies' interpretation from models of thin beds and horizontal circular cylinders (spheres) in complex environments (oblique magnetization, rugged relief and unknown levels of the normal magnetic field) using improved versions of characteristic points and tangents was presented in detail in the author's previous publications. However, many geological targets have a geometrical form of thick beds and thin horizontal plates and intermediate forms that crop up between these two models. In this paper, a methodology for interpreting magnetic anomalies produced by thick bed models in complex environments is explicitly described. It shows that quantitative analysis of magnetic anomalies due to intermediate targets could be successfully carried out using the methodology developed for the thick bed model. In the case of a thin horizontal plate with a large horizontal size, two distinct anomalies (from the left and right ends) may be interpreted as anomalies from thin beds. The interpretation methodology was successfully tested, both on typical models and on real geological targets. It was concluded that these methods could be effectively applied for quantitative analysis of magnetic surveys for geological-geophysical mapping, archeological target delineation, ore body searching, revealing oil and gas traps, and solving other geological and environmental problems.
机译:磁勘探是一种快速,廉价的地球物理工具,是全世界地球物理勘探最广泛使用的方法之一。但是,诸如倾斜磁化,研究区域复杂的地质结构以及不平坦的地形起伏之类的噪声因素严重掩盖了观测到的磁异常的解释。详细介绍了在复杂环境(倾斜磁化,凹凸起伏和未知水平的法向磁场)中使用薄层和水平圆柱(球体)模型解释磁异常的方法,并使用了改进的特征点和切线形式在作者以前的出版物中。但是,许多地质目标的几何形式是厚床层和薄水平板,而中间形式则出现在这两个模型之间。在本文中,明确描述了解释复杂环境中厚床模型产生的磁异常的方法。结果表明,可以使用针对厚床模型开发的方法成功地对由于中间目标而引起的磁异常进行定量分析。对于水平尺寸较大的薄水平板,两个不同的异常(从左端和右端)可以解释为薄层异常。解释方法已在典型模型和实际地质目标上成功测试。得出的结论是,这些方法可有效地用于地质勘探,地质目标标定,矿体搜索,揭示油气藏以及解决其他地质和环境问题的电磁勘探定量分析。

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