Electrical Structure of the Earth's Upper Mantle

地球上地幔的电结构

• 批准号: 9526651
• 负责人: Mark Everett
• 金额: $ 10.17万
• 依托单位: Texas A&M Research Foundation
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1996
• 资助国家: 美国
• 起止时间: 1996-02-15 至 1999-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9526651&HistoricalAwards=false
• 关键词: Electrical; Structure; Earth; Upper; Mantle

Everett 9526651 Constraints on the large-scale structure of Earth's upper mantle from global seismic tomography, plate motion reconstructions, and regional tomographic studies on the fate of subducting slabs influence our view of convection in the planet. The evidence supports large-scale, volumetric lateral heterogeneity in the upper mantle, in addition to internal discontinuities at 410 and 660 km. Long-period electromagnetic induction data from the worldwide magnetic observatory network can resolve large-scale lateral variations in mantle structure. The PI proposes to develop and apply a spherical 3-d inversion scheme for imaging lateral variations in upper mantle conductivity of the earth. The inversion will be based on the PI's recently developed spherical finite element code. Using the inversion code, and constrains from other geophysical techniques, the PI proposes to 1) test the hypothesis that long period global induction data are consistent with upper mantle seismic tomographic results, 2) develop a regularization algorithm and invert the global induction data set for the three-dimensional electrical conductivity structure of the upper mantle, and 3) incorporate galvanic and oceanic effects into the existing forward model of electromagnetic induction in a heterogeneous sphere. The proposed work is likely to lead to useful progress on 3-d modeling and interpretation of mantle conductivity variations and provide independent constraints on mantle dynamics.

全球地震层析成像对地球上地幔大尺度结构的制约，板块运动重建，以及对俯冲板块命运的区域层析研究，埃弗雷特9526651影响了我们对地球对流的看法。除了410公里和660公里处的内部不连续外，证据还支持上地幔存在大规模的、体积上的横向不均质性。来自全球地磁观测网的长周期电磁感应数据可以解决地幔结构的大范围横向变化。国际地球物理研究所建议开发和应用一种球面三维反演方案，用于成像地球上地幔电导率的横向变化。反演将基于PI最近开发的球面有限元程序。利用反演程序和其他地球物理技术的约束，PI建议1)检验长周期全球感应数据与上地幔地震层析成像结果一致的假设，2)开发正则化算法并反演上地幔三维电导率结构的全球感应数据集，3)将电流和海洋效应纳入现有的非均匀球体电磁感应正演模型。拟议的工作可能导致在地幔电导率变化的三维模拟和解释方面取得有益的进展，并对地幔动力学提供独立的约束。