正版 精化岩石圈结构的重力测量方法 (捷克)罗伯特 滕策(Robert

“地球物理基础丛书”序
Preface
Summary
Chapter 1 Introduction
Chapter 2 Coordinate Systems and Transformations
Chapter 3 Earth's Gravity Field

Chapter 4 Earth's Density Model
4．1 2-D Density Model
4．2 3-D Density Model
4．3 Concluding Remarks

Chapter 5 Examples of Density Models
5．1 Seawater Density Model
5．1．1 Data Acquisition and TEOS-10
5．1．2 Seawater Density Distribution
5．1．3 Accuracy Analysis
5．1．4 Concluding Remarks
5．2 Marine Sediment Density Model
5．2．1 Marine Sediment Data
5．2．2 Methodology
5．2．3 Numerical Analysis and Results
5．2．4 Model Uncertainties
5．2．5 Concluding Remarks
5．3 Ocean-Sediment and Sediment-Bedrock Density Inter{ace
5．3．1 Methodology
5．3．2 Input Data
5．3．3 Results
5．3．4 Concluding Remarks

Chapter 6 Earth's Crustal Density Model
6．1 Methodology and Datasets
6．2 ESCM180 Spectrum
6．3 ESCM180 Spectral Characteristics
6．4 Average Density of Crustal Structures
6．5 Concluding Remarks

Chapter 7 Gravimetric Forward Modeling
7．1 Gravitational Field of 3-D Mass Density Layer
7．2 Gravitational Field of Radially-Varying Mass Density Layer
7．3 Gravitational Field of Laterally-Varying Mass Density Layer
7．4 Gravitational Field of Uniform Mass Density Layer
7．5 Concluding Remarks

Chapter 8 Gravitational Field of Crustal Structures
8．1 Methodology
8．2 Results
8．3 Correlation Analysis
8．4 Spectral Analysis
8．5 Concluding Remarks

Chapter 9 Gravitational Model of Oceanic Lithosphere
9．1 Methodology
9．2 Data Acquisition
9．3 Synthetic Gravitational Model
9．4 Validation of Results
9．5 Concluding Remarks

Chapter 10 Gravimetric Moho Recovery
10．1 Global Moho Recovery
10．1．1 Spectral Functional Model
10．1．2 Compensation Attraction
10．2 Moho Solution for Variable Moho Density Contrast
10．2．1 Functional Model
10．2．2 Compensation Attraction
10．3 Regional Moho Recovery
10．3．1 Discrete Functional Model
10．3．2 Discretization
10．4 Concluding Remarks

Chapter 11 Global Gravimetric Moho Model
11．1 Consolidated Crust-Stripped Gravity Disturbances
11．2 Moho Density Contrast
11．3 Mantle Gravity Disturbances
11．4 Moho Solutions
11．5 Validation of Results
11．6 Spectral Analysis
11．7 Correlation Analysis
11．8 Concluding Remarks

Chapter 12 Sub-Crustal Stress Field
12．1 Horizontal Sub-Crustal Stress
12．2 Vening Meinesz-Moritz Isostatic Model
12．3 Combined Model
12．4 Convergence Analysis
12．5 Concluding Remarks

Chapter 13 Terrestrial Sub-Crustal Stress Field
13．1 Global Sub-Crustal Stress Study
13．2 Regional Sub-Crustal Stress Studies
13．2．1 Stress Field Along Oceanic Subductions Zones
13．2．2 Stress Field at Hotspots
13．2．3 Stress Field Along Tectonic Plate Boundaries
13．2．4 Stress Field Along Continent-to-Continent Collision Zones
13．3 Concluding Remarks

Chapter 14 Martian Sub-Crustal Stress Field
14．1 Martian Topography
14．2 Martian Free-Air Gravity Field
14．3 Martian Bouguer Gravity Field
14．4 Martian Crustal Thickness
14．5 Martian Sub-Crustal Stress
14．5．1 Global Stress Field
14．5．2 Signature of Impact Craters
14．5．3 Signature of Hemispheric Dichotomy
14．5．4 Signature of Ice Load
14．5．5 Spectral Analysis of Stress Field
14．5．6 Long-Wavelength Stress Field
14．5．7 Tharsis Stress Field
14．6 Concluding Remarks
References

评论

《精化岩石圈结构的重力测量方法（英文版）》研究岩石圈密度结构重力解释方法，特别是壳幔（莫霍面）密度界面重力测定法。提出了地球动力学现象与地幔对流有关重力的解释方法，即对海底扩张的签名和重力场中的子地壳应力。这些功能模型利用的球形谐波分析和合成的引力场和岩石圈密度结构的方法。这些方法的实际应用进行数值研究地球的球面地壳密度模型计算，主要地壳密度结构的重演，大洋岩石圈的综合引力模型编制，解决发现莫霍面深度的重力反问题，和子的地壳应力场的测定。