Structure of the Tibetan Crust and Upper Mantle and Its Geodynamic Implications

青藏高原地壳和上地幔的结构及其地球动力学意义

• 批准号: 0337622
• 负责人: Michael Ritzwoller
• 金额: $ 23.91万
• 依托单位: University of Colorado at Boulder
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2004
• 资助国家: 美国
• 起止时间: 2004-01-01 至 2007-12-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0337622&HistoricalAwards=false
• 关键词: Structure; Tibetan; Crust; Upper; Mantle

This research will study the large-scale structure of the crust and upper mantle beneath Tibet andinvestigate its geodynamic implications. Two features of a preliminary 3-D seismic model motivate this work and define the primary questions that the work proposes to address.First, a coherent 3-D pattern of high and low speed anomalies in the mantle underlies the Tibetan plateau. What geodynamic processes can account for this pattern? Second, strong mid-crustal radial anisotropy characterizes the Tibetan crust, and preliminary analysis implies coherent, period-dependent azimuthal anisotropy. Which models of the development of finite strain in the Tibetan crust are consistent with these observations?The work will improve the current seismic model and investigate its geodynamical implications.The model will be improved by adding more surface wave dispersion measurements and by introducing new kinds of measurements into the inversion; e.g., crustal and mantle overtone measurements and receiverfunctions. The inversion generates an ensemble of acceptable models, rather than a single best-fitting model, thereby producing meaningful uncertainty information needed to test hypotheses. Several geodynamic scenarios that may explain aspects of the pattern of velocity anomalies in the upper mantlebeneath Tibet will be investigated, including; the underthrusting of Indian lithosphere, southwestwardthrusting of Asian lithosphere, and the detachment or convective removal of Tibetan lithosphere.In addition, the relation between inferred crustal anisotropy and three models of the development of finitestrain in the Tibetan crust will be investigated.A graduate student will receive training at the interface between seismic tomography andgeodynamics. The seismic models will be placed in a form that is useful in the classroom. Collaborators in this effort include researchers at the Digital Library for Earth Systems Education (DLESE, www.dlese.org) and UNAVCO, who are also part of the GEON large scale information technology research project (www.geongrid.org).

这项研究将研究西藏地壳和上地幔的大尺度结构，并探讨其地球动力学意义。初步的三维地震模型的两个特征激发了这项工作，并确定了工作要解决的主要问题：第一，青藏高原下方地幔中高速和低速异常的一致三维模式。什么样的地球动力学过程可以解释这种模式？其次，强烈的中地壳径向各向异性是西藏地壳的特征，初步分析表明，相干的、与周期有关的方位各向异性。西藏地壳有限应变发展的哪些模型与这些观测结果一致？这项工作将改进现有的地震模型，并研究其地球动力学含义。通过增加更多的面波频散测量和在反演中引入新的测量方法，例如地壳和地幔泛音测量和接收函数，将改进该模型。反演产生一个可接受的模型集合，而不是单一的最佳拟合模型，从而产生检验假设所需的有意义的不确定性信息。将研究几种可能解释西藏下地幔速度异常模式的地球动力学情景，包括印度岩石圈的俯冲，亚洲岩石圈的西南向冲，以及西藏岩石圈的剥离或对流移动。此外，还将研究推断的地壳各向异性与西藏地壳有限运动发展的三种模式之间的关系。一名研究生将在地震层析成像与地球动力学的界面上接受培训。地震模型将以一种在课堂上有用的形式放置。这项工作的合作者包括地球系统教育数字图书馆(DLESE，www.dlese.org)和联合国志愿人员组织的研究人员，他们也是Geon大规模信息技术研究项目(www.geongrid.org)的一部分。