<p> </p><ul><li>1.1 Background and Research Objectives</li><li>1.2 Importance of Studying High-Pressure Metamorphic Rocks</li><li>1.3 Scope and Research Questions</li><li>1.4 Significance for Tectonic and Lithospheric Evolution</li><li>1.5 Thesis Organization</li></ul> <ul><li>2.1 Concepts in High-Pressure Metamorphism</li><li>2.2 Petrological and Mineralogical Characteristics</li><li>2.3 Previous Studies on Petrogenesis of High-Pressure Rocks</li><li>2.4 Analytical Techniques in Petrological Analysis</li><li>2.5 Theoretical Framework</li></ul> <ul><li>3.1 Selection of Study Areas with High-Pressure Rocks</li><li>3.2 Fieldwork and Sample Collection</li><li>3.3 Petrological and Mineralogical Analysis Techniques</li><li>3.4 Thermodynamic Modeling Approaches</li><li>3.5 Data Integration for Pressure-Temperature Paths</li></ul> <ul><li>4.1 Petrographic Characteristics of High-Pressure Rocks</li><li>4.2 Identification of Mineral Assemblages and Textures</li><li>4.3 Pressure-Temperature-Time Evolution Models</li><li>4.4 Comparison with Regional Tectonic Framework</li><li>4.5 Implications for Tectonic Processes</li></ul> <ul><li>5.1 Summary of Petrogenetic Findings</li><li>5.2 Contributions to High-Pressure Metamorphic Studies</li><li>5.3 Limitations and Suggestions for Future Research</li><li>5.4 Practical Implications for Tectonic Reconstructions</li><li>5.5 Recommendations for Further Research and Collaborations</li></ul> <br><p></p>