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大陆地震科学考察及相关研究(英文版)


作者:
Yong-Gang Li, Yongxian Zhang, Zhongliang Wu, Ying Li, and Xiaodong Zhang
定价:
198.00元
ISBN:
978-7-04-064874-4
版面字数:
310.00千字
开本:
16开
全书页数:
暂无
装帧形式:
精装
重点项目:
暂无
出版时间:
2025-06-13
物料号:
64874-00
读者对象:
学术著作
一级分类:
自然科学
二级分类:
地球科学
三级分类:
地球物理学

暂无
  • 前辅文
  • 1 Scientific Investigation of Continental Earthquakes and Relevant Studies: An Overview
    • References
  • 2 Crustal Deformation and Regional Seismogenic Environment Associated with the 2021 Maduo MW7.3 Earthquake
    • 2.1 Introduction
    • 2.2 Calculation of GNSS Velocity Field and Strain Rate Field
      • 2.2.1 GNSS Observation and Data Processing
      • 2.2.2 Method for Calculating GNSS Strain Rate Field
    • 2.3 Characteristics of Crustal Deformation and Fault Activity of Regional GNSS
    • 2.4 Regional GNSS Strain Accumulation Characteristics
    • 2.5 Co-seismic Deformation Characteristics from Continuous GNSS Observations
    • 2.6 Deformation Characteristics of Station QHMD in the Early Post-Seismic Period
    • 2.7 Distribution Characteristics and Trend Analysis of Great Earthquakes on the Boundary Faults of Bayan Har Block
    • 2.8 Conclusion
    • References
  • 3 Dense Array Observation and Deep Seismogenic Environment in the Focal Area of the 2021 Maduo MS7.4 Earthquake, Qinghai, China
    • 3.1 Dense Seismic Array Observation
    • 3.2 High-Resolution Earthquake Catalog for the Focal Area of the Maduo MS7.4 Earthquake Sequence Based on Deep-Learning Phase Picker and Dense Array
      • 3.2.1 Workflow of Phase Picking, Association, Absolute and Relative Location
      • 3.2.2 The Temporal Distribution Characteristics of Earthquake Sequences
      • 3.2.3 The Spatial Distribution Characteristics of Earthquake Sequences and the Fault Morphology
    • 3.3 Focal Mechanism Solutions of the Maduo MS7.4 Earthquake Sequence and Regional Stress Field of Focal Region
      • 3.3.1 Focal Mechanism Solutions
      • 3.3.2 The Stress Field
    • 3.4 Three-Dimensional Fine Velocity Structure of the Upper Crust of the 2021 Maduo MS7.4 Earthquake
    • 3.5 Variations of Shear Wave Splitting in the Focal Area of the Maduo MS7.4 Earthquake
    • 3.6 Conclusion
    • References
  • 4 Seismotectonic Settings and Seismogenic Mechanism of the 2021 MS6.0 Luxian Induced Earthquake in the Sichuan Basin, Eastern Tibetan Plateau
    • 4.1 Introduction
    • 4.2 Tectonic and Geological Settings
    • 4.3 Focal Mechanisms and Seismicity Relocation
      • 4.3.1 Focal Mechanisms
      • 4.3.2 Seismicity Relocation
    • 4.4 The Ambient Stress Field
    • 4.5 Geological and Seismic Investigation
    • 4.6 Geodetic Observations
    • 4.7 Velocity Structures and the Seismic Distribution Characteristics
    • 4.8 Discussion and Conclusion
      • 4.8.1 Seismogenic Fault of the Luxian Strong Earthquake
      • 4.8.2 Seismotectonic Settings of the Southern Sichuan Basin
      • 4.8.3 Future Perspectives
    • References
  • 5 Gas Emissions Associated with Strong Earthquakes in the Intersection Area of Longmenshan, Xianshuihe and Anninghe Faults, Southwestern China
    • 5.1 Introduction
    • 5.2 Tectonic Setting
    • 5.3 Data andMethod
      • 5.3.1 Data
      • 5.3.2 Method
    • 5.4 Results and Discussion
      • 5.4.1 The Background Around the Kangding Area
      • 5.4.2 Gas Emissions from the Fault Zone and Epicenter Area
      • 5.4.3 Gas Emissions Associated with Strong Earthquakes
    • 5.5 Conclusion
    • References
  • 6 Operational Aftershock Forecasting Work for Scientific Investigation Activities of China Earthquake Administration in Recent Years
    • 6.1 Introduction
    • 6.2 Earthquake Sequences Employed
    • 6.3 Methodology
      • 6.3.1 Epidemic Type Aftershock Sequence (ETAS) Model
      • 6.3.2 Receiver Operating Characteristic (ROC) Test
      • 6.3.3 Consistency Test
    • 6.4 Results and Discussion
      • 6.4.1 Temporal Variation of Aftershock Sequence
      • 6.4.2 Forecasting Probability and Occurrence Rate
      • 6.4.3 ROC and Consistency Test with Observations
    • 6.5 Conclusion
    • References
  • 7 Predictability of the May 12, 2008, Wenchuan Earthquake: Insights from the Perspective of ‘Dragon King’ Theory and ‘Nowcasting’ Method
    • 7.1 Introduction
    • 7.2 Earthquake Catalogues Used for the Analysis
    • 7.3 Predictability of the Wenchuan Earthquake in the Perspective of ‘Dragon King’ Theory
    • 7.4 Hazard of the Wenchuan Earthquake in the Perspective of ‘Nowcasting’
    • 7.5 Conclusions and Discussion
    • References
  • 8 Nowcasting Earthquakes with QuakeGPT:Methods and First Results
    • 8.1 Introduction
    • 8.2 Continuous Time Earthquake Nowcasting with ROC Methods
      • 8.2.1 Method
      • 8.2.2 Exponential Moving Average (EMA)
      • 8.2.3 Nowcasting with California Earthquakes
    • 8.3 Stochastic Simulation: Earthquake Rescaled Aftershock Seismicity “ERAS”
      • 8.3.1 Stochastic Simulations of Seismicity
      • 8.3.2 ERAS: General Approach
      • 8.3.3 Examples of ERAS Catalog Simulations and Comparison with California Data
    • 8.4 Science Transformers: AI Enhanced Time Series Forecasting
    • 8.5 QuakeGPT: A Generative Pretrained Earthquake Transformer
      • 8.5.1 Earthquake Transformers and QuakeGPT
      • 8.5.2 ERAS Earthquake Simulations
      • 8.5.3 Transformer Architecture
      • 8.5.4 Queries, Keys and Values
    • 8.6 Summary and Discussion
    • Appendix: Building the ERAS Model
    • References
  • 9 Falsification of Seismic Hazard Assessment (SHA) by Real Earthquakes: The Design Magnitude Mdesign for Neo-deterministic Seismic Hazard Assessment (NDSHA)
    • 9.1 DSHA andMCE
    • 9.2 Mdesign in NDSHA: The Panza-Rugarli Law
      • 9.2.1 MCE and Its Clarification
      • 9.2.2 The Safety Factor of Earthquake Magnitude, γEM
      • 9.2.3 The Magnitude Standard Deviation, σM
      • 9.2.4 Principle of Uniformitarianism
    • 9.3 NDSHA Procedures, and the Role of Mdesign
    • 9.4 Falsification of NDSHA Through the Mdesign
    • 9.5 Conclusions and Discussion
    • References
  • 10 Numerical Investigations and Observations of Waveguide Effects for Multi-layer Fault Damage Zones at Seismogenic Depths
    • 10.1 Introduction
    • 10.2 The SimulationMethod
    • 10.3 3-D Finite-Difference Simulations of FZTWs
      • 10.3.1 Simulations of FZTWs for Sources Within the Four-Layer LVWG
      • 10.3.2 Simulations of FZTWs for Sources 2-km Out of the Four-Layer LVWG
      • 10.3.3 Simulations of FZTWs for Sources Beneath the Two-Layer LVWG
      • 10.3.4 Simulations of FZTWs for Sources Within and Out of the Uniform LVWG
    • 10.4 Observations and Simulations of FZTWs from Multi-layered Fault Damage Zones
      • 10.4.1 FZTWS at the Landers and Hect Mine Rupture Zones
      • 10.4.2 FZTWs at the San Andreas Fault Near SAFOD Site
    • 10.5 Conclusion and Discussion
    • References
  • 11 Detailed Investigation of Seismic Hazardous Areas and Scientific Field Investigation of Earthquakes: A Discussion from the Perspective of Systems Engineering
    • 11.1 Detailed Investigation of Seismic Hazardous Areas: Current Status
    • 11.2 Detailed Investigation of Seismic Hazardous Areas and Scientific Field Investigation of Earthquakes: The Scientific Significance
    • 11.3 Planning the Detailed Investigation of Seismic Hazardous Areas and the Scientific Field Investigation of Earthquakes
      • 11.3.1 Basic Principles
      • 11.3.2 PriorityWorks
    • 11.4 Capacity Building for the Detailed Investigation of Seismic Hazardous Areas and the Scientific Field Investigation of Earthquakes: A Long-Term Plan for Their Modernization
      • 11.4.1 The First to the Third Year: The Pilot Phase of the Modernization
      • 11.4.2 The Fourth to the Fifth Year: System Construction and Optimization
    • 11.5 Working Projects
      • 11.5.1 Project Objectives
      • 11.5.2 Project Content
      • 11.5.3 Expected Results of the Project
    • 11.6 Towards an Organization on the International Inter-disciplinary Investigation of Earthquakes

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