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Applicability of moment tensor inversions to mine-induced microseismic data.

机译:矩张量反演对矿山诱发的微地震数据的适用性。

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摘要

The seismic moment tensor is a valuable tool in the evaluation of seismic source mechanisms, because it is the most general representation of any indigenous source. For that reason, a seismic moment-tensor inversion approach has been developed by E. S. G. Canada Inc. for retrieval of source mechanisms of mine-induced microseismic data. This method is unique because it is based on a time-domain calculation/evaluation of the seismic moment-tensor components. It is important to realise that this waveform inversion software is quite sophisticated and intricate due to the many levels of coding which implement the numerical, graphical and interactive aspects. In this thesis, a waveform simulation program is developed as a means to test the limitations and applicability of this moment-tensor inversion method. The simulation algorithm produces relatively simple seismic signals not unlike "ideal" mine-induced microseismic waveforms. These simulated waveforms, however, are sophisticated enough to test the inversion approach for the retrieval of geometrical as well as shear and nonshear components of failure.;The inversion method is also tested on real data from the Underground Research Laboratory (Pinawa, Manitoba), in order to verify the approach with observational limitations. (Abstract shortened by UMI.)
机译:地震矩张量是评估地震震源机制的重要工具,因为它是任何本地震源的最一般表示。因此,E.S.G.Canada Inc.开发了一种地震矩-张量反演方法,以检索地雷引起的微地震数据的源机制。该方法是独特的,因为它基于地震矩张量分量的时域计算/评估。重要的是要意识到,由于实现数字,图形和交互方面的许多编码级别,该波形反转软件非常复杂和复杂。本文开发了一种波形仿真程序,以测试该矩张量反演方法的局限性和适用性。模拟算法产生相对简单的地震信号,与“理想的”地雷诱发的微地震波形不同。但是,这些仿真波形非常复杂,足以测试用于获取故障的几何以及剪切和非剪切分量的反演方法。还对地下研究实验室(马尼托巴省皮纳瓦)的真实数据进行了反演方法的测试,为了验证该方法在观察上的局限性。 (摘要由UMI缩短。)

著录项

  • 作者

    Angus, Douglas A. C.;

  • 作者单位

    Queen's University (Canada).;

  • 授予单位 Queen's University (Canada).;
  • 学科 Geophysics.
  • 学位 M.Sc.
  • 年度 1999
  • 页码 104 p.
  • 总页数 104
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:48:16

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