首页> 外文会议>CPS/SEG(Society of Exploration Geophysicists) 2004 International Geophysical Conference: Expanded Abstracts vol.2; 2004; >High-speed computation of gravity and magnetic anomalies in 3-D inversion for physical properties
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High-speed computation of gravity and magnetic anomalies in 3-D inversion for physical properties

机译:高速反演3维反演中重力和磁异常的物理性质

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A currently prevailing approach in gravity and magnetic inversion, especially in 3-D case is regularly subdividing the source region into a set of juxtaposed cuboids, and estimating the physical properties of the cuboids by using an inversion of potential field, and deducing the image of the geological sources. If nonlinear global methods used in the inversion, the paper shows that there exists an excessive computation that has bottlenecked the effectiveness of the methods. Several special tricks have been taken to break the choke point of overwhelming computation, one of which is to separate the geometric trellis from formulas. The trellis is invariable during the whole process of inversion, and can be stored as a table, which would make the following reiterative forwardcompu-tation as just a simple reading of the table and multiplying it with corresponding properties of the geometric cells. The caused huge storage of geometric trellis has been tremendously reduced by a very skill of e-quivalent storing. The approaches revive the nonlinear methods in their applications to the inversion of gravity and magnetic anomalies for 3-D physical properties.
机译:目前在重力和磁反演(尤其是在3-D情况下)中流行的方法是将源区域定期细分为一组并列的长方体,并通过使用势场反演来估算长方体的物理性质,并推导出地质来源。如果在反演中使用非线性全局方法,则表明存在过多的计算,从而限制了方法的有效性。已经采取了几种特殊的技巧来打破压倒性计算的瓶颈,其中之一就是将几何网格与公式分开。网格在整个反演过程中是不变的,并且可以存储为表格,这将使以下的迭代正向计算成为表格的简单读取,并将其乘以几何单元的相应属性。相当数量的电子等效存储技术极大地减少了造成的几何格架的巨大存储量。这些方法使非线性方法在3D物理属性的重力和磁异常反演中的应用得以复兴。

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