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大地测量联合反演理论和方法研究进展 被引量:16

Progress of Joint Inversion on Geodesy and Geophysics
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摘要 综述了 1 0多年来国内外大地测量反演问题研究的成果及最新进展 ,特别是大地测量联合反演模型、大地测量联合反演算法以及大地测量联合反演理论和方法在研究地壳运动、地球构造等中的应用成果 ,讨论了联合卫星测高、声纳测深及海洋激光雷达遥感信息反演海洋环境参量 ,联合INSAR、GPS和水准资料反演研究地壳运动和联合各种观测数据反演研究地球内部构造问题。随着科学技术的发展 ,大地测量联合反演理论和方法研究将在监测全球变化、防灾减灾、发展地球科学理论方面取得更大进展。 The achievement and new progress in geodesy and geophysical inversion in the recent decade are summerized in this paper.There are many models of geodesy joint inversion based on mechanical pattern.The model identification is preliminarily discussed.Developing an inverse analysis model based on the Global deformation data is presented in IAG2001.Various local optimization methods and global optimization methods (like genetic algorithm and IA algorithm) are developed. The numerical manifold method (NMM) is also introduced into geodesy joint inversion.Both the finite element method (FEM) for continual and the discontinuous deformation analysis (DDA) for block systems are special cases of this numerical manifold method. We can estimate bottom ocean topography with gravity data using the integrated inverse method,obtain the complete horizontal motions within zones of distributed deformation from the inversion of strain rate data and study recent crustal deformation and strain accumulations inferred from GPS and seismicity data.We can also detect active fault segment with joint inversion of observed gravity and GPS baseline changes and study the crustal movements with various observations including geodetic,geological and seismic.
作者 许才军
出处 《武汉大学学报(信息科学版)》 EI CSCD 北大核心 2001年第6期555-561,共7页 Geomatics and Information Science of Wuhan University
基金 国家自然科学基金资助项目 ( 4 990 40 0 1) 教育部高等学校骨干教师资助计划资助项目 ( 2 0 0 0 3)
关键词 联合反演理论 地壳运动 地球介质参数 海洋环境参量 大地测量学 joint inversion theory crustal movement medium parameter ocean environment parameter
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