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Three-dimensional deformation and stress models of the Death Valley and San Andreas Fault Zones.

机译:死亡谷和圣安地列斯断层带的三维变形和应力模型。

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摘要

Crustal deformation studies of tectonic motions have been the topic of many scientific investigations, as they can provide critical information about how tectonic structures shape and deform the Earth. While crustal deformation studies using observational data alone can provide a great deal of information about how the Earth is presently deforming, it is standard practice to implement mathematical and physics-based models to investigate the underlying causes of deformation in the crust. These models, constrained by geological, geodetic and seismic data, have successfully contributed key constraints of ongoing deformation processes and have provided predictions of past and future tectonic behavior of the Earth. One of the most popular regions of study on Earth is the San Andreas Fault System (SAFS), as it provides an ideal environment for investigating the deformation caused by a major continental transform boundary. Furthermore, the Death Valley Fault Zone (DVFZ) is an ideal area to study large-scale crustal deformation due to its well-exposed features related to progressive extensional deformation.;This dissertation presents new information about the deformation, stress accumulation rates, and strain rates taking place in the DVFZ and SAFS using three-dimensional (3-D) crustal deformation models. Chapter 1 provides the background and motivation of the modeling work applied to both fault systems. Chapter 2 provides the results obtained from applying a 3-D semi-analytic viscoelastic model constrained by GPS measurements to explore the kinematics and stress accumulation in the DVFZ. Chapter 3 analyzes the influence of intrusions on the motion and deformation of the DVFZ through a finite difference modeling approach. Chapter 4 explores the strain rate distribution within the SAFS, assuming a dipping fault geometry for its southern segments, utilizing a modified 3-D semi-analytic viscoelastic model. Lastly, Chapter 5 gives a description of the future work that may be followed based on the results obtained from this dissertation work.
机译:构造运动的地壳形变研究一直是许多科学研究的主题,因为它们可以提供有关构造结构如何塑造和变形地球的重要信息。虽然仅使用观测数据进行的地壳变形研究就可以提供有关地球目前如何变形的大量信息,但通常的做法是实施基于数学和物理的模型来调查地壳变形的根本原因。这些模型受地质,大地测量和地震数据的约束,成功地贡献了正在进行的变形过程的关键约束,并提供了对地球过去和未来构造行为的预测。 San Andreas断层系统(SAFS)是地球上最受欢迎的研究区域之一,因为它为调查由主要大陆变换边界引起的变形提供了理想的环境。此外,死亡谷断层带(DVFZ)由于具有与渐进式伸展变形有关的良好特征,因此是研究大规模地壳变形的理想区域。本论文提供了有关变形,应力累积率和应变的新信息。使用三维(3-D)地壳变形模型在DVFZ和SAFS中进行速度变化。第1章提供了应用于两个故障系统的建模工作的背景和动机。第2章提供了通过应用受GPS测量约束的3-D半解析粘弹性模型来研究DVFZ中的运动学和应力累积的结果。第三章通过有限差分建模方法分析了入侵对DVFZ运动和变形的影响。第四章探讨了SAFS内的应变率分布,假设其南部段具有断层断层几何形状,并使用改进的3-D半解析粘弹性模型。最后,第5章根据从本论文工作获得的结果,对以后的工作进行了描述。

著录项

  • 作者

    Del Pardo, Cecilia.;

  • 作者单位

    The University of Texas at El Paso.;

  • 授予单位 The University of Texas at El Paso.;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 162 p.
  • 总页数 162
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 语言学;
  • 关键词

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