...
首页> 外文期刊>Earth, planets and space: EPS >2D inversion of 3D magnetotelluric data: The Kayabe dataset
【24h】

2D inversion of 3D magnetotelluric data: The Kayabe dataset

机译:3D大地电磁数据的2D反演:Kayabe数据集

获取原文
获取原文并翻译 | 示例
           

摘要

In the last two Magnetotelluric Data Interpretation Workshops (MT-DIW) the participants were asked to model the Kayabe magnetotelluric dataset, a dense (100 m) grid of thirteen lines, with thirteen stations in each line. Bahr's phase-sensitive skew and the Groom and Bailey decomposition were used to select those lines for which the data could be considered two-dimensional. For these lines we used a 2D inversion algorithm to obtain a series of resistivity models for the earth. Finally, we constructed a 3D model using the 2D models and critically examined the validity and practicality of this approach based on 3D model study. We found that in the Kayabe dataset case the common practice of using 2D models to depict 3D models, can only be used to create a starting model for 3D interpretation. The sequential 2D models as a representation of a 3D body is unacceptable in terms of fit to the observed data. We question the validity of some of the conductivity structures in the 2D models, as they can be mere artifacts created by the algorithm to match 3D effects.
机译:在最近的两个大地电磁数据解释研讨会(MT-DIW)中,要求参与者对Kayabe大地电磁数据集进行建模,该数据集是由13条线组成的密集(100 m)网格,每条线中有13个站点。使用Bahr的相敏偏斜以及Groom和Bailey分解来选择那些可以将数据视为二维的线。对于这些线,我们使用了2D反演算法来获得一系列针对地球的电阻率模型。最后,我们使用2D模型构建了3D模型,并基于3D模型研究严格审查了该方法的有效性和实用性。我们发现,在Kayabe数据集案例中,使用2D模型描绘3D模型的常见做法只能用于创建3D解释的起始模型。以连续2D模型作为3D物体的表示形式,不适合所观察的数据。我们对2D模型中某些电导率结构的有效性提出质疑,因为它们仅是算法为匹配3D效果而创建的人工产物。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号