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  • 1
    Call number: S 99.0139(354)
    In: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover, Nr. 354
    Type of Medium: Series available for loan
    Pages: 155 Seiten , Illustrationen, Diagramme, Karten
    ISBN: 978-3-7696-5252-9 , 9783769652529
    ISSN: 0065-5325
    Series Statement: Wissenschaftliche Arbeiten der Fachrichtung Geodäsie und Geoinformatik der Leibniz Universität Hannover Nr. 354
    Language: English
    Note: Dissertation, Gottfried Wilhelm Leibniz Universität Hannover, 2019 , 1. Introduction 1.1. Research Objectives 1.2. Outline and Structure of the Thesis 2. Theoretical Background 2.1. Introduction 2.2. SAR Imaging 2.2.1. SAR Image Distortions 2.2.2. SAR Imaging Modes 2.2.3. SAR Missions 2.3. SAR Interferometry 2.3.1. InSAR Workflow 2.3.2. InSAR Decorrelation 2.3.3. Errors in InSAR 2.3.4. Examples of Interferograms 2.3.5. Decomposition of Line-of-Sight Measurements 2.4. Multi Temporal InSAR 2.4.1. Scattering Mechanisms in SAR Images 2.4.2. Interferogram Stacking 2.4.3. Persistent Scatterer InSAR 2.4.4. Small Baseline InSAR 2.5. Analysis of Displacement Time Series 2.5.1. Continuous Wavelet Transform 2.5.2. Cross Wavelet Transform 2.5.3. Application of CWT and XWT to InSAR Time Series 3. Methodological Contribution 37 3.1. Introduction 3.2. Challenges in Large-scale InSAR 3.3. Proposed Method 3.3.1. Interferogram Formation 3.3.2. Adaptive Correction of Interferograms 3.3.3. Estimating the Displacement Rate 3.3.4. Estimating the Time Series of Displacement 4. InSAR Monitoring of Localized Landslide in Taihape, New Zealand 4.1. Abstract 4.2. Introduction 4.3. Study Area 4.4. Methods 4.4.1. InSAR Measurement 4.4.2. Ancillary Data 4.4.3. Cause-Effect Analysis 4.5. Results 4.5.1. Small-baseline Interferograms 4.5.2. Time-series Results 4.6. Discussion 4.6.1. Suitability of InSAR Measurements for Monitoring the Taihape Landslide 4.6.2. Interpretation of InSAR Results 4.6.3. Comparison with Ground Truth 4.6.4. Comparison with Rainfall and Groundwater Level 4.7. Conclusion 4.8. Acknowledgments 4.9. Supplementary Materials 5. InSAR Measurement of Regional Land Subsidence in Tehran, Iran 5.1. Abstract 5.2. Introduction 5.3. Study Area and Problem Description 5.4. Datasets 5.4.1. SAR Data 5.4.2. Leveling 5.4.3. Groundwater Level 5.5. Methods 5.5.1. Multi-temporal InSAR Analysis 5.5.2. Merging InSAR Time Series 5.5.3. Cause-Effect Analysis 5.6. Results 5.6.1. Southwest of Tehran 5.6.2. IKA Airport 5.6.3. Varamin County 5.6.4. Time Series of Displacement 5.6.5. Accuracy, Precision and Consistency Assessments 5.7. Discussion 5.7.1. Structural Control of the Displacement 5.7.2. Comparison with Groundwater 5.7.3. Elastic vs. Inelastic Compaction 5.8. Conclusion 5.9. Acknowledgments 5.10. Supplementary materials 5.10.1. Significance of Tropospheric Delay 5.10.2. Decomposition of LOS Measurement 5.10.3. Under/Overestimation of Displacement Rates 6. Sentinel-1 InSAR Measurement of Anthropogenic Deformation in Germany 6.1. Summary 6.2. Introduction 6.3. Sentinel-1 InSAR Processing 6.4. Large-scale Sentinel-1 Processing 6.5. Anthropogenic Ground Motion in Berlin 6.6. Mining-induced Deformation in Leipzig 6.7. Conclusions and Prospect 6.8. Acknowledgements 7. Subsequent Work: Measurement of Localized Deformations over Extensive Areas 7.1. Introduction 7.2. SAR Datasets 7.3. Sentinel-1 Interferograms 7.4. Corrected Interferograms 7.5. Displacement Maps and Time Series 7.6. Discussion 7.7. Conclusion 8. Cooperation Works 8.1. Quantifying Land Subsidence in the Rafsanjan Plain, Iran Using InSAR Measurements 8.1.1. Abstract 8.1.2. Author Contribution 8.2. Characterizing Post-construction Settlement of Masjed-Soleyman Dam Using TerraSAR-X SpotLight InSAR 8.2.1. Abstract 8.2.2. Author Contribution 8.3. InSAR Observation of the 18 August 2014 Mormori (Iran) Earthquake 8.3.1. Author Contribution 9. Summary and Future Work 9.1. Future works , Zusammenfassung in Englisch und Deutsch Seite 3-6
    Location: Lower compact magazine
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  • 2
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    In:  J. Geophys. Res., Amsterdam, Univ. Tokyo, vol. 105, no. B7, pp. 16,341-16,358, pp. B12306, (ISSN: 1340-4202)
    Publication Date: 2000
    Keywords: Induced seismicity ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Rheology ; 1236 ; Geodesy ; and ; gravity ; Rheology ; of ; the ; lithosphere ; and ; mantle ; (8160) ; 3210 ; Mathematical ; geophysics ; (new ; field) ; Modeling ; 8015 ; Structural ; geology ; (new ; field, ; replaces ; single ; entry ; 8165) ; Local ; crustal ; structure ; 8159 ; Tectonophysics ; Rheology--crust ; and ; lithosphere ; JGR
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  • 3
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    In:  Bull. Seism. Soc. Am., Reykjavík, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 92, no. 4, pp. 1377-1389, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 2002
    Keywords: Earthquake ; USA ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Satellite Laser Ranging ; Geodesy ; BSSA ; Jonsson
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  • 4
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    In:  Geophys. Res. Lett., Luxembourg, EGS-Gauthier-Villars, vol. 29, no. 12, pp. 47-1 to 47-4, pp. 1606
    Publication Date: 2002
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; SAR ; Volcanology ; GRL ; 8414 ; Volcanology: ; Eruption ; mechanisms ; 8419 ; Eruption ; monitoring ; (7280) ; 8494 ; Instruments ; and ; techniques ; 1206 ; Geodesy ; and ; Gravity: ; Crustal ; movements--interplate ; (8155)
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  • 5
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    In:  Science, University of Iceland, Icelandic Meteorological Office, Ministry for the Environment,, vol. 310, no. 5753, pp. 1473-1476, pp. 1567, (ISBN: 0534351875, 2nd edition)
    Publication Date: 2005
    Keywords: Rheology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; USA ; Geol. aspects ; long-term ; 1915 ; 1954 ; Basin ; and ; Range ; Wasatch ; fault ; InSAR
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  • 6
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    In:  Geophys. Res. Lett., Washington, D.C., AGU, vol. 31, no. 7, pp. 1669-1675, pp. L07622, (ISSN: 1340-4202)
    Publication Date: 2004
    Keywords: Stress ; Coulomb ; Volcanology ; Seismicity ; Fault plane solution, focal mechanism ; GRL ; FROTH ; TWALTER
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  • 7
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    In:  J. Geophys. Res., Washington, D.C., AGU, vol. 110, no. B10, pp. 1669-1675, pp. B10205, (ISSN: 1340-4202)
    Publication Date: 2005
    Keywords: TWALTER ; FROTH
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  • 8
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    In:  J. Geophys. Res., Washington, D.C., AGU, vol. 111, no. B5, pp. 1669-1675, pp. B05204, (ISSN: 1340-4202)
    Publication Date: 2006
    Keywords: Volcanology ; Seismicity ; USA ; static ; elastic ; Stress ; JGR ; volcano ; spreading ; dike ; intrusion ; 8414 ; Volcanology: ; Eruption ; mechanisms ; and ; flow ; emplacement ; 8415 ; Intra-plate ; processes ; (1033, ; 3615) ; 8425 ; Effusive ; volcanism ; 8439 ; Physics ; and ; chemistry ; of ; magma ; bodies ; 8488 ; Volcanic ; hazards ; and ; risks ; TWALTER
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  • 9
    Publication Date: 2016-06-24
    Description: We use ALOS-1 Interferometric Synthetic Aperture Radar data spanning the period of 2007-2011 to obtain time-dependent ground deformation data over all of the volcanoes in Colombia, Ecuador and Peru. We detect deformation on or near the proximity of Galeras, Reventador, Tungurahua, Guagua Pichincha, Sangay, and Cerro Auquihuato volcanoes, uncovering previously undocumented deformation in the latter three. Deformation is attributed to changes in pressurization of the volcanic systems (Galeras, Tungurahua, Guagua Pichincha, and Cerro Auquihuato), subsidence associated with flow deposits (Reventador), and flank creep (Sangay). Our models suggest that the pressure sources are located at depths of ∼1 to 6 km from the surface, indicating that the measurable deformation within our data is restricted to shallow magma chambers and hydrothermal systems. This article is protected by copyright. All rights reserved.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 10
    Publication Date: 2016-07-23
    Description: We use 2004-2011 Envisat Synthetic Aperture Radar (SAR) imagery and InSAR time-series methods to estimate the contemporary rates of strain accumulation in the Chaman Fault system in Pakistan and Afghanistan. At 29 N we find long-term slip rates of 16 ± 2.3 mm/yr for the Ghazaband Fault and of 8 ± 3.1 mm/yr for the Chaman Fault. This makes the Ghazaband Fault one of the most hazardous faults of the plate boundary zone. We further identify a 340 km-long segment displaying aseismic surface creep along the Chaman Fault, with maximum surface creep rate of 8.1 ± 2 mm/yr. The observation that the Chaman Fault accommodates only 30% of the relative plate motion between India and Eurasia implies that the remainder is accommodated south and east of the Katawaz block microplate.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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