利用低阶大地水准面异常反演大尺度核幔边界起伏

崔荣花; 方剑; 刘杰; 李红蕾; 陈铭

doi:10.13203/j.whugis20150577

利用低阶大地水准面异常反演大尺度核幔边界起伏

崔荣花^{1, 2,},
方剑¹,
刘杰^{1, 3},
李红蕾^{1, 2},
陈铭^{1, 2}

1.
中国科学院测量与地球物理研究所大地测量与地球动力学国家重点实验室, 湖北武汉, 430077
2.
中国科学院大学, 北京, 100049
3.
河南理工大学测绘与国土信息工程学院, 河南焦作, 454000

基金项目:

国家重点基础研究发展计划（973计划） 2013CB733301

详细信息

作者简介:
崔荣花, 博士生, 主要从事地球重力场研究。rhcui@asch.whigg.ac.cn

中图分类号: P223
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出版历程
- 收稿日期: 2016-04-30
- 发布日期: 2018-05-04

Using Lower Degrees of Geoid Anomalies to Invert Large Scale Undulations of Core-Mantle Boundary

CUI Ronghua^{1, 2,},
FANG Jian¹,
LIU Jie^{1, 3},
LI Honglei^{1, 2},
CHEN Ming^{1, 2}

1.
State Key Laboratory of Geodesy and Eaerh's Dynamics, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China
2.
University of Chinese Academy of Sciences, Beijing 100049, China
3.
School of Surveying and Land Information Engineering, Henan Polytechnic University, Jiaozuo 454000, China

Funds:

>The National Program on Key Basic Researth Project of China(973 Program) 2013CB733301

More Information

Author Bio:
CUI Ronghua, PhD candidate, specializes in Earth's gravity field. E-mail: rhcui@asch.whigg.ac.cn

摘要

摘要: 核幔边界（core-mantle boundary，CMB）是地球内部最重要的物理化学界面之一，地核和地幔通过核幔边界发生多种相互作用，这对地球重力场、地球自转及地磁场等都能产生重要影响。大地水准面异常是地球重力场的重要观测量，反映了地球内部的物质密度异常及界面变化等重要信息。推导了通过大地水准面异常反演核幔边界起伏的公式，利用2~4阶大地水准面异常反演了大尺度核幔边界起伏形态。结果显示，核幔边界起伏的径向幅度达±5 km、与Morelli的地震层析成像结果的幅度接近，但在形态上略有差异。以高为5 km、底边长为1 000 km的棱柱体模型模拟计算了核幔边界密度异常引起的大地水准面异常响应，结果与观测大地水准面异常比较接近。
- 大地水准面异常 /
- 核幔边界起伏 /
- 层析成像 /
- 地球重力场
Abstract: The core-mantle boundary (CMB) is one of the most important physical and chemical interfaces in the earth's interior, through which a variety of interactions occur between Earth's core and mantle. These interactions might have great impacts on Earth's gravity field, rotation and magnetic field. The geoid anomalies is an important observation of the earth's gravity field, which reflects significant information of the earth's interior, such as material density anomalies and interfaces, etc. A formula using the geoid anomalies to invert undulations of core-mantle boundary was derived. The large-scale undulations of the core-mantle boundary were calculated by this formula from degree 2 to 4. The result showed that the amplitude of core-mantle boundary undulations reached ±5 km, which corresponded to that obtained by Morelli using seismic tomography, but showed some differences in the worldwild distribution. We also simulated influences of the density anomalies in the core-mantle boundary to the geoid undulation using a prism model with height of 5 km and base length of 1 000 km. The result showed that it was closed to the observed value of geoid undulations.
- geoid anomalies /
- core-mantle boundary undulations /
- seismic tomography /
- Earth's gravity field

HTML全文

图 1 全球5~12阶大地水准面异常和全球板块构造

Figure 1. Global Geoid Anomalies from Degree 5 to 12 and Global Plate Tectonics

下载: 全尺寸图片幻灯片

图 2 2-4阶全球大地水准面起伏

Figure 2. Global Geoid Undulation from Degree 2 to 4

下载: 全尺寸图片幻灯片

图 3 由大地水准面起伏计算的核幔边界起伏

Figure 3. Undulation of CMB Computed by Geoid Undulation

下载: 全尺寸图片幻灯片

图 4 核幔边界高5 km的棱柱体质量异常计算的地表大地水准面异常

Figure 4. Map of Geoid Undulation Computed by a Prism Mass Anomaly with a Height of 5km Located on Core-Mantle Boundary

下载: 全尺寸图片幻灯片

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