Constraining Two Prominent Low-Velocity Anomalies in the Lower Mantle beneath Africa and Pacific
Constraining Two Prominent Low-Velocity Anomalies in the Lower Mantle beneath Africa and Pacific
批准号:
0309859
负责人:
Lianxing Wen
金额:
$20.83万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2003
资助国家:
美国
项目状态:
已结题
起止时间:
2003-09-01 至 2007-08-31
中文摘要
研究人员建议绘制非洲和太平洋下地幔两个显著低速异常的详细结构和速度特征图。他将使用2D混合方法进行广泛的波形建模,使用不同的地震震相来约束来自不同方向的地震异常的地震速度、几何形状和长度-尺度。PI还建议在该研究计划的过程中开发一种三维混合地震代码。三维混合程序将用于正演验证二维混合方法波形模拟所获得的地震结果的有效性。该提议的学术价值包括地震学的观测和理论两个方面。该提议的观测方面包括收集、识别、解释和模拟高质量的异常地震数据,其科学目标是绘制下地幔两个显著低速异常的详细特征图。该提案的理论方面包括对地震波在非均匀地幔中传播的系统研究,对异常地震数据的详细模拟,以及开发3D混合方法。该研究对进一步认识地球的形成演化、地幔中的热化学对流、核幔边界的性质以及“杜帕尔异常”等地球化学储集体的成因具有广泛的意义。新的3D代码将在地震界有广泛的应用。
英文摘要
WenThe investigator proposes to map out detailed structural and velocity features of the two prominent low-velocity anomalies in the lower mantle beneath Africa and the Pacific. He will use extensive waveform modeling by the 2D hybrid methods to constrain the seismic velocities, geometry, and length-scale of the seismic anomalies from various directions using various seismic phases. The PI also proposes to develop a three-dimensional hybrid seismic code along the course of this research program. The three-dimensional hybrid code will be used to forward verify the validity of the seismic results obtained from the 2D-hybrid method waveform modeling. The intellectual merits of the proposal include both observational and theoretical aspects of seismology. The observational aspect of the proposal includes collection, identification, interpretation and modeling of high-quality anomalous seismic data, with a scientific goal of mapping detailed features of the two prominent low-velocity anomalies in the lower mantle. The theoretical aspect of the proposal includes systematic studies of seismic wave propagation in a heterogeneous mantle, detailed modeling of the anomalous seismic data, and the development of a 3D hybrid method. The proposed research has broad impacts on our further understanding of the formation and evolution of the Earth, thermal-chemical convection in the mantle, the nature of the core-mantle boundary, and the origin of some geochemical reservoirs, such as "the DUPAL anomaly". The new 3D code will have broad applications in the seismology community.
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会议论文
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