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CRUST-MANTLE THERMAL STRUCTURE AND TECTONOTHERMAL EVOLUTION OF THE TIBETAN PLATEAU


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CRUST-MANTLE THERMAL STRUCTURE AND TECTONOTHERMAL EVOLUTION OF THE TIBETAN PLATEAU
  • 书号：7030052714
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  • 所属分类：P54 构造地质学
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目录

  • Foreword
    Preface
    Chapter Ⅰ A Brief Outline of Previous Studies Relevant to the Tibetan Tectonothermal Evolution
    Ⅰ.1 Mosaic Accretionary Structure and Terrane Amalgamation History of the Tibetan Plateau
    Ⅰ.1.1 Terrane Division and Accretionary Structure of the Tibetan Plateau
    Ⅰ.1.2 An Outline of the Terrane Amalgamation History
    Ⅰ.2 Thick Tibetan Crust and the Characteristic Geophysical Fields of the Thickened Crust and Lithosphere
    Ⅰ.2.1 Seismic Wave Velocity Structure of the Thickened Tibetan Crust
    Ⅰ.2.2 Density Structure of the Thickened Tibetan Crust Revealed by Gravimetric Observations
    Ⅰ.2.3 Information from Magnetic Survey
    Ⅰ.2.4 Information from Magnetotelluric Sounding
    Ⅰ.3 Neotectonism,Terrane Deformations and Integrated Uplift-Evolution of the Tibetan Plateau
    Ⅰ.3.1 Neotectonism on the Tibetan Plateau
    Ⅰ.3.2 Forms and Dynamics of Deformation of the Tibetan Lithosphere
    Ⅰ.3.3 Integrated Uplift-Evolution of the Tibetan Plateau
    Chapter Ⅱ Results of Heat Flow Measurements on the Tibetan Plateau and Their Quality Evaluation
    Ⅱ.1 Bottom-lake Heat Flow Measurements in South-Tibet and the Heat Flow Corrections
    Ⅱ.1.1 Heat Flow Measurements in South-Tibetan Lakes
    Ⅱ.1.2 Main Results of Bottom-lake Heat Flow Measurements
    Ⅱ.1.3 Summarization and Classification of the Heat Flow Corrections
    Ⅱ.1.4 Correction for the Lake Bottom Temperature Fluctuations
    Ⅱ.1.5 Steady-state Corrections to the Heat Flow Values Observed at Lake Bottom
    Ⅱ.1.6 Non-Steady-state Corrections
    Ⅱ.2 Borehole Heat Flow Measurements in Some Geothermal Areas in Central Tibet
    Ⅱ.2.1 Deep-seated Conductive Heat Flow Measurement in the Yangbajain Geothermal Field
    Ⅱ.2.2 Conductive-convective or Pure Convective Heat Flow Measurements in Other Geothermal Areas
    Ⅱ.3 Heat Flow Measurements Along the Yadong-Golmud Geoscience Transect
    Ⅱ.3.1 Conductive Heat Flow Measurements in the Southern and Northern Bordering Areas of the Lhasa-Gangdise Terrane
    Ⅱ.3.2 Conductive Heat Flow Measurements in the Pre-Himalayan Old Terranes in the Northern Part of the Tibetan Plateau
    Ⅱ.4 Quality Evaluation of the Observed Borehole Heat Flow Values
    Chapter Ⅲ Heat Flow Distribution Pattern and the Crust-Mantle Thermal Structure of the Tibetan Plateau
    Ⅲ.1 Distribution Pattern of the Observed Surface Heat Flow Along the Yadong-Golmud Geoscience Transect Across the Tibetan Plateau
    Ⅲ.2 Theoretical Verification of a Multi-layered Crust-Mantle Thermal Structure Model in the Southern Part of the Tibetan Plateau
    Ⅲ.2.1 Theme Background
    Ⅲ.2.2 Crust-Mantle Thermal State of the Converging Plates
    Ⅲ.2.3 Controlling Effect of the Shallow Heat Source Body on the Surface Heat Flow Distribution
    Ⅲ.2.4 Preliminary Crust-Mantle Thermal Structure of Southern Tibet
    Ⅲ.2.5 A Case Study of the Yangbajain Geothermal Field Demonstrating the Thermal Structure of the Uppermost Crust in the Himalayan Geothermal Belt
    Ⅲ.2.6 A Brief Summary
    Ⅲ.3 The N-S Heterogeneity of the Crust-Mantle Thermal Structure on the Tibetan Plateau
    Ⅲ.3.1 Cold Stable Block of Amalgamated Old Terranes in the North
    Ⅲ.3.2 Tectonically Heated Lhasa-Gangdise Terrane of Compressional Deformation Origin in the Middle
    Ⅲ.3.3 Gradually Heated Himalayan Terrane of Southward Mobile Extension Type in the South
    Ⅲ.4 Steady-state Crust and Mantle Temperature Simulation of the Tibetan Plateau
    Ⅲ.4.1 Theme Background
    Ⅲ.4.2 Geometrical Dimensions and Thermophysical Parameter Selection in the Steady-state Thermal Modelling
    Ⅲ.4.3 Results of Steady-state Crust-Mantle Temperature Simulation
    Chapter Ⅳ Methodology of the Study on the Integrated Tectonothermal Evolution of the Tibetan Plateau
    Ⅳ.1 Importance and Tasks of the Model Simulation of the Integrated Tectonothermal Evolution Process
    Ⅳ.2 Guidelines and Principles in Designing the Tectonothermal Evolution Model
    Ⅳ.2.1 Division of the Research Stages in the Integrated Tectonothermal Evolution Model Study
    Ⅳ.2.2 Principles and Guidelines of Designing the Tectonothermal Evolution Model
    Ⅳ.2.3 Methodology and Steps of the Model Study
    Chapter Ⅴ Tectonic Framework of the 3D Terrane Deformations Constrained by the Surface Uplift History
    Ⅴ.1 Plate-converging Velocity Model of the Tectonic Evolution of the Tibetan Plateau
    Ⅴ.2 Derivation of the Kinematic-geometrical Equations of Tectonic Deformations for the Lhasa-Gangdise Terrane
    Ⅴ.2.1 Shortening Terrane Length L(t)and Total Mass Loss ∫(S＋E)dt
    Ⅴ.2.2 Cumulative Mass Loss Rate by Erosion δe(t)
    Ⅴ.2.3 Cumulative Lateral Mass Transfer Rate δs(t)
    Ⅴ.2.4 Increasing Crustal Thickness D(t)in Consideration of Mass Loss and Transfer
    Ⅴ.2.5 Cumulative Horizontal Shortening Σl(t)Caused by Lateral Extension and Strike-slip Movement
    Ⅴ.2.6 Simultaneously Increasing Lithospheric Thickness M(t)in Consideration of Mass Transfer
    Ⅴ.2.7 Tectonic Height of Uplifted Surface H(t)Accompanying Crustal Thickening
    Ⅴ.2.8 Isostatic Height of Surface Hi(t)of the Thickened and Uplifted Crust
    Ⅴ.2.9 A Brief Summarization
    Ⅴ.3 Derivation of the Kinematic-geometrical Equations of Tectonic Deformations for the Himalayan Terrane
    Ⅴ.3.1 Length of the Deformation Domain L(t)in the Newly Formed Terrane
    Ⅴ.3.2 Cumulative Mass Loss by Erosion ∫ E(t)dt
    Ⅴ.3.3 Increasing Crustal Thickness D(t)of the Newly Formed Terrane at the Convergence Boundary in Consideration of Mass Loss by Erosion
    Ⅴ.3.4 Simultaneously Increasing Lithospheric Thickness M(t)at the Convergence Boundary
    Ⅴ.3.5 Tectonic Height of Uplifted Surface H(t)of the Newly Formed Terrane at the Convergence Boundary
    Ⅴ.3.6 Increasing Crustal Thickness Ds(t),Increasing Lithospheric Thickness Ms(t)and Tectonic Height Hs(t)at the Commonly Accepted Terrane Boundary
    Ⅴ.3.7 A Brief Summarization
    Ⅴ.4 Tibetan Uplift History and Its Constraining Implications for the Verification and Refinement of the Selected Tectonic Evolution Framework of the Tibetan Plateau
    Ⅴ.4.1 Theme Background
    Ⅴ.4.2 Summarization of a Representative Tibetan Uplift History
    Ⅴ.4.3 Intrinsic Aspects in the Tibetan Uplift Process
    Ⅴ.4.4 An Improved Kinematics-uplift Model Used as the Ultimate Surface Constraint on the Tectonic Evolution Framework
    Chapter Ⅵ Simulation of the Integrated Tectonothermal Evolution and the Main Results
    Ⅵ.1 Intrinsic Thermal Processes and Responses Induced by Tectonic Deformations
    Ⅵ.1.1 The Enhancement of Intracrustal Radiogenic Self-heating During the Crustal Shortening and Thickening
    Ⅵ.1.2 Strain-heating During Terrane Deformations
    Ⅵ.1.3 Friction Heating and Shear Strain-friction Heating Along Faults
    Ⅵ.1.4 The Enforcement of Basal Heating During Lithospheric Thinning due to Basal Delamination
    Ⅵ.1.5 The Heat Absorption Effect During Rock Melting
    Ⅵ.1.6 Temperature Field Disturbance by Hypabyssal Emplacement of Crust-originated Magma
    Ⅵ.2 Methodology of the Tectonothermal Simulation and the Model Parameters
    Ⅵ.3 Main Results of Simulation of the Integrated Tectonothermal Evolution of Terranes
    Ⅵ.3.1 The Evolutionary Trend of the Crust and Mantle Temperature Field
    Ⅵ.3.2 Thermal Evolution Histories of Terranes
    Ⅵ.3.3 Contemporary Crust and Mantle Temperature Distribution in the Tibetan Terranes
    Ⅵ.3.4 Evolutionary Trend of the Surface Heat Flow in the Deforming Terranes on the Tibetan Plateau
    Conclusions
    References
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