基于站点独立grom - bailey分解的PNG数据集一维模型研究

H. Toh, M. Uyeshima
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引用次数: 5

摘要

巴布亚新几内亚(PNG)数据集的传统大地电磁(MT)分析表明,它是一个非常好的二维(2D)数据集,具有相对较高的信噪比(S/N),最高可达10.2 S。然而,传统Swift的角度在某些站点上是不稳定的,并且在站点之间略有不同。这意味着所有场址都存在微弱但明显的扭曲。因此,在七个选定的地点,通过最小化由与地点和频率无关的grom - bailey (GB)分解得出的全局x2错配来寻求区域2D走向角。其余3个位点经x2检验淘汰。走向角确定为地理北偏西60°。利用分解的二维主张量元素的Berdichevsky平均值进行一维(1D)蒙特卡罗反演。仅基于一维反演的二维模型能够再现观测到的阻抗,除了TM相位在10 -1至10 s的周期范围内具有系统的高值。这表明,该区域下的电导率结构的一维近似是合理有效的。一维模型表明,地表以下存在一层薄(高达2.5公里)的电阻层,表明存在“单一”的达拉石灰岩。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
One-Dimensional Model Study of the PNG Dataset Using Site-Independent Groom-Bailey Decomposition
Conventional magnetotelluric (MT) analyses of the Papua New Guinea (PNG) dataset reveal that it is a very good two-dimensional (2D) dataset with relatively high S/N ratios up to 10 2 s. However, traditional Swift's angles are unstable at some sites and differ slightly site to site. This implies that weak but significant distortions are present at all sites. Hence, the regional 2D strike angle was sought by minimizing the global X 2 misfits derived from the site- and frequency-independent Groom-Bailey (GB) decomposition at seven selected sites. The other three sites were eliminated by X 2 -test. The strike angle was determined to be 60° west of geographic north. One-dimensional (1D) Monte-Carlo inversion was performed using the Berdichevsky averages of the decomposed 2D principal tensor elements. The 2D model simply based on the 1D inversions was able to reproduce the observed impedances, except for the systematically high values of TM phase in the period range of 10 -1 to 10 s. This indicates that a 1D approximation of the electrical conductivity structure beneath this region is reasonably valid. The 1D models indicated the existence of a thin (up to 2.5 km) resistive layer just below the surface, suggesting the 'single' Darai limestone.
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