Based on the analysis of impedance tensor data, tipper data, and the conjugate gradient algorithm, we develop a three-dimensional （3D） conjugate gradient algorithm for inverting magnetotelluric full information data...Based on the analysis of impedance tensor data, tipper data, and the conjugate gradient algorithm, we develop a three-dimensional （3D） conjugate gradient algorithm for inverting magnetotelluric full information data determined from five electric and magnetic field components and discuss the method to use the full information data for quantitative interpretation of 3D inversion results. Results from the 3D inversion of synthetic data indicate that the results from inverting full information data which combine the impedance tensor and tipper data are better than results from inverting only the impedance tensor data （or tipper data） in improving resolution and reliability. The synthetic examples also demonstrate the validity and stability of this 3D inversion algorithm.展开更多
The Ordos block is a stable tectonic unit since the Cenozoic. Whether low-resistivity layers exist in the middle and lower crust of this kind block is an open question. This work attempts to reveal the entire crustal ...The Ordos block is a stable tectonic unit since the Cenozoic. Whether low-resistivity layers exist in the middle and lower crust of this kind block is an open question. This work attempts to reveal the entire crustal structure of the block based on interpretation of magnetotelluric data collected along the profile across this region. The result shows that a layered structure characterizes the crust of the Ordos block, with a low-resistivity layer at depth of about 20km, presumably associated with fluids there. In contrast, in the areas of active tectonics on the east and west of the block, there are no such layered electric structures in the crust, and the low-resistivity zones may be related to the decollement zones (or ductile shear zones) in the crust. The difference in electric structure of crust between the Ordos Block and neighboring areas is of significance to analyze the movement and deformation of varied blocks in the continent.展开更多
针对当前地球物理勘探数据库系统一系列普遍存在的问题,如专业数据结构设计的复杂性、对数据处理加工要求和缺乏对专项成果数据的有效管理,开展了基于深部探测岩石圈结构的大地电磁测深成果数据库设计与实现。本课题以大地电磁测深基本...针对当前地球物理勘探数据库系统一系列普遍存在的问题,如专业数据结构设计的复杂性、对数据处理加工要求和缺乏对专项成果数据的有效管理,开展了基于深部探测岩石圈结构的大地电磁测深成果数据库设计与实现。本课题以大地电磁测深基本理论、数据库技术和计算机技术为基础,收集以深部探测为主的全国各大区域大地电磁测深资料,并对其进行整理、分析和建模,设计与开发基于SQL Server 2005和Visual Basic 6.0的大地电磁数据库系统。该系统不仅可快捷地实现数据的检索、查询、编辑、输入、输出等基本功能,而且可进行大地电磁成果图件的存取和可视化操作。同时,本系统的研发将对开展中国岩石圈结构、地球动力学和地球构造演化的研究起到重要的技术支撑作用。展开更多
基金supported by the National Hi-tech Research and Development Program of China（863Program）（No.2007AA09Z310） National Natural Science Foundation of China（Grant No.40774029 40374024）+1 种基金 the Fundamental Research Funds for the Central Universities（Grant No.2010ZY53） the Program for New Century Excellent Talents in University（NCET）
文摘Based on the analysis of impedance tensor data, tipper data, and the conjugate gradient algorithm, we develop a three-dimensional （3D） conjugate gradient algorithm for inverting magnetotelluric full information data determined from five electric and magnetic field components and discuss the method to use the full information data for quantitative interpretation of 3D inversion results. Results from the 3D inversion of synthetic data indicate that the results from inverting full information data which combine the impedance tensor and tipper data are better than results from inverting only the impedance tensor data （or tipper data） in improving resolution and reliability. The synthetic examples also demonstrate the validity and stability of this 3D inversion algorithm.
基金sponsored by Earthquake Research Project for Public Affair(2008419010)the National Natural Science Foundation of China(40374032, 40534023)+4 种基金the Basic Scientific Research Special Program of the Institute of Geology,CEA(DFIGCEA0607117)the Basic Scientific Research Fund of the State Level Institutes for Commonweal (DF-IGCEA-0607-1-17)the National Basic Research Program(2004CB418402),Chinathe National Key Basic Research Program (95-13-02-02)the Key Program of the Natural Science Foundation of China (40534023)
文摘The Ordos block is a stable tectonic unit since the Cenozoic. Whether low-resistivity layers exist in the middle and lower crust of this kind block is an open question. This work attempts to reveal the entire crustal structure of the block based on interpretation of magnetotelluric data collected along the profile across this region. The result shows that a layered structure characterizes the crust of the Ordos block, with a low-resistivity layer at depth of about 20km, presumably associated with fluids there. In contrast, in the areas of active tectonics on the east and west of the block, there are no such layered electric structures in the crust, and the low-resistivity zones may be related to the decollement zones (or ductile shear zones) in the crust. The difference in electric structure of crust between the Ordos Block and neighboring areas is of significance to analyze the movement and deformation of varied blocks in the continent.
文摘针对当前地球物理勘探数据库系统一系列普遍存在的问题,如专业数据结构设计的复杂性、对数据处理加工要求和缺乏对专项成果数据的有效管理,开展了基于深部探测岩石圈结构的大地电磁测深成果数据库设计与实现。本课题以大地电磁测深基本理论、数据库技术和计算机技术为基础,收集以深部探测为主的全国各大区域大地电磁测深资料,并对其进行整理、分析和建模,设计与开发基于SQL Server 2005和Visual Basic 6.0的大地电磁数据库系统。该系统不仅可快捷地实现数据的检索、查询、编辑、输入、输出等基本功能,而且可进行大地电磁成果图件的存取和可视化操作。同时,本系统的研发将对开展中国岩石圈结构、地球动力学和地球构造演化的研究起到重要的技术支撑作用。
