(Downloads - 0)
For more info about our services contact : help@bestpfe.com
Table of contents
1. INTRODUCTION
Contributions
Thesis Roadmap
2. BRIEF REVIEW OF LITERATURE
2.1 The Earthquake Cycle
2.1.1 Interseismic period
2.2.1 Aseismic creep and seismic potential
2.3 The North Anatolian Fault (NAF)
2.3.1 Postseismic creep along the North Anatolian Fault
2.4 Ground Subsidence
3. METHODOLOGY
3.1 Introduction
3.2 Principles of InSAR
3.2.1 Contributors to signal phase
3.3 Overcoming Limitations due to Decorrelation Noise
3.4 Persistent Scatterer Method (PS)
3.4.1 Procedures: from SLC to geocoded interferograms
3.4.2 Procedures: from Interferograms to PS time-series
4. SHALLOW CREEP ALONG THE 1999 IZMIT EARTHQUAKE RUPTURE (TURKEY) FROM GPS AND HIGH TEMPORAL RESOLUTION INSAR DATA
4.1 Introduction
4.2 GPS Data and Processing
4.3 InSAR Data and Methodology
4.3.1 Multi-sensor insar time-series
4.3.2 PS-InSAR Processing
4.4 Results
4.4.1 Mean Line-of-Sight Velocity Fields
4.4.2 Fault-parallel horizontal velocities versus vertical velocities
4.4.3 Horizontal Creep Rate Distribution Along Fault
4.4.4 Vertical Motion Along the 1999 Rupture
4.5 Modelling Profile Velocities
4.6 Temporal Evolution of Creep
4.7 Discussion
4.7.1 Spatial Distribution of Creep and Geometrical and Lithological Control
4.7.2 High Temporal Resolution InSAR Data Reveal Burst-Like Behavior of Creep
4.8 Conclusion
5. ANALYSIS OF SECULAR GROUND MOTIONS IN ISTANBUL FROM LONG-TERM INSAR TIME_SERIES (1992-2017)
5.1 Introduction
5.2 Background of Study Areas
5.2.1 Geological setting
5.2.2 Study Area 1: Haramidere valley and Avcilar neighborhood
5.2.3 Study Area 2: Ayamama river valley
5.3 Datasets
5.4 Results and Discussion
5.4.1 Main deformation patterns
5.4.2 Site 1 : Haramidere valley
5.4.3 Site 2 : Ayamama river
5.4.4 Sites 4, 6 and 3
5.4.5 Site 5
5.5 Conclusion
6. INVESTIGATING SUBSIDENCE IN THE BURSA PLAIN, TURKEY, WITH SATELLITE RADAR INTERFEROMETRY
6.1 Introduction
6.2 Study Area
6.3 Datasets
6.4 Deformation Decomposition of Sentinel -1 Data
6.5 Results
6.5.1 InSAR-derived land subsidence maps
6.6 Discussion
6.6.1 Impact of the looking geometry on self-consistency checking between the ascending and descending InSAR observations
6.6.2 Water table variations and InSAR time series
6.6.4 Compressibility of the aquifer in the Bursa plain
6.6.3 Lithological and tectonic control over land subsidence
6.7 Conclusion
7. CONCLUSIONS AND PERSPECTIVES
REFERENCES
APPENDICES
CURRICULUM VITAE
