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Simultaneous estimation of total magnetization direction and 3-D spatial orientation

机译:同时估算总磁化方向和3-D空间方向

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摘要

Magnetic interpretations are usually carried out either by assuming induced magnetization and estimating the model geometry, or by presuming a known source spatial orientation to estimate the total magnetization. We present a 3-D magnetic interpretation method that estimates simultaneously the total magnetization direction and the spatial orientation of the source. It is based on the approximation of the anomaly by the series derived from expanding the magnetic potential into multipoles and retaining source moments up to second order. The moments and linear combinations of moments appearing in the series are then inverted from the magnetic anomaly. The total magnetization is assumed constant in direction but not in magnitude. It is also presumed implicitly that the anomalous distribution of magnetization intensity has nonzero values in a finite-volume region, is far from the observation points, and presents three othogonal planes of symmetry intersecting at the center of the dipole moment. The method is essentially linear and requires no a priori explicit assumption of a fixed geometry for the sources. The method is particularly suited to interpret compact, isolated or disjoint, but spatially correlated sources. If the source satisfies all assumptions presumed by the method, it is possible to obtain accurate, stable estimates of the total dipole moment vector, the position of the center of dipole moment, and the directions of all three principal axes of symmetry. If the source is not far from the observation plane and/or if the total magnetization direction is not constant, it is still possible to obtain accurate and stable estimates of the direction of the mean total magnetization and the projection, on the observation plane, of the center of dipole moment. The method is applied to magnetic data from the Gulf of Guinea Seamount. The estimated magnetic palaeopole is at 50°48′S and 74°54′E which is in good agreement with estimates published by other authors.
机译:磁性解释通常通过假设感应磁化强度和估算模型几何形状,或通过假定已知的源空间方位来估算总磁化强度来进行。我们提出了一种3-D磁性解释方法,该方法可以同时估算源的总磁化方向和空间方向。它基于通过将磁势扩展为多极并保持源矩直至二阶而得出的级数对异常的近似。然后,将序列中出现的力矩和力矩的线性组合从磁异常中反转。假定总磁化强度在方向上恒定,但大小上不固定。还隐含地假定,磁化强度的反常分布在有限体积区域中具有非零值,远离观察点,并且呈现出在偶极矩中心相交的三个正交对称平面。该方法本质上是线性的,不需要先验明确假设光源的固定几何形状。该方法特别适合于解释紧凑,孤立或不相交但空间相关的源。如果源满足该方法假定的所有假设,则可以获取总偶极矩矢量,偶极矩中心位置和所有三个对称主轴方向的准确,稳定的估计值。如果源距观测平面不远和/或总磁化方向不恒定,则仍可能获得平均总磁化方向的准确且稳定的估计以及观测平面上的投影。偶极矩的中心。该方法适用于来自几内亚湾海山的磁数据。估计的古古磁极在50°48′S和74°54′E处,这与其他作者发表的估算值非常吻合。

著录项

  • 来源
    《Geophysics》 |1995年第5期|p.1365-1377|共13页
  • 作者单位

    Dept. Fisica/CCE, Federal University of Rio Grande do Norte, Caixa Postal 1641, CEP 59.072-970, Natal, RN Brazil;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地球物理学;
  • 关键词

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