Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway
Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old depos...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Li, Zhihai [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2021transfer abstract |
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| Übergeordnetes Werk: |
Enthalten in: Islamic finance development and banking ESG scores: Evidence from a cross-country analysis - Paltrinieri, Andrea ELSEVIER, 2019, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:377 ; year:2021 ; day:15 ; month:03 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1016/j.geomorph.2020.107586 |
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| 520 | |a Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. | ||
| 520 | |a Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. | ||
| 700 | 1 | |a Wang, Qing |4 oth | |
| 700 | 1 | |a Zhou, Fujun |4 oth | |
| 700 | 1 | |a Li, Yuchao |4 oth | |
| 700 | 1 | |a Han, Xudong |4 oth | |
| 700 | 1 | |a Mehmood, Qaiser |4 oth | |
| 700 | 1 | |a Cao, Chen |4 oth | |
| 700 | 1 | |a Gu, FeiFan |4 oth | |
| 700 | 1 | |a Han, Mengxia |4 oth | |
| 700 | 1 | |a Chen, Jianping |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Paltrinieri, Andrea ELSEVIER |t Islamic finance development and banking ESG scores: Evidence from a cross-country analysis |d 2019 |g Amsterdam [u.a.] |w (DE-627)ELV003279995 |
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10.1016/j.geomorph.2020.107586 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001299.pica (DE-627)ELV053105982 (ELSEVIER)S0169-555X(20)30559-6 DE-627 ger DE-627 rakwb eng 650 VZ Li, Zhihai verfasserin aut Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway 2021transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Wang, Qing oth Zhou, Fujun oth Li, Yuchao oth Han, Xudong oth Mehmood, Qaiser oth Cao, Chen oth Gu, FeiFan oth Han, Mengxia oth Chen, Jianping oth Enthalten in Elsevier Science Paltrinieri, Andrea ELSEVIER Islamic finance development and banking ESG scores: Evidence from a cross-country analysis 2019 Amsterdam [u.a.] (DE-627)ELV003279995 volume:377 year:2021 day:15 month:03 pages:0 https://doi.org/10.1016/j.geomorph.2020.107586 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U AR 377 2021 15 0315 0 |
| spelling |
10.1016/j.geomorph.2020.107586 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001299.pica (DE-627)ELV053105982 (ELSEVIER)S0169-555X(20)30559-6 DE-627 ger DE-627 rakwb eng 650 VZ Li, Zhihai verfasserin aut Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway 2021transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Wang, Qing oth Zhou, Fujun oth Li, Yuchao oth Han, Xudong oth Mehmood, Qaiser oth Cao, Chen oth Gu, FeiFan oth Han, Mengxia oth Chen, Jianping oth Enthalten in Elsevier Science Paltrinieri, Andrea ELSEVIER Islamic finance development and banking ESG scores: Evidence from a cross-country analysis 2019 Amsterdam [u.a.] (DE-627)ELV003279995 volume:377 year:2021 day:15 month:03 pages:0 https://doi.org/10.1016/j.geomorph.2020.107586 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U AR 377 2021 15 0315 0 |
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10.1016/j.geomorph.2020.107586 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001299.pica (DE-627)ELV053105982 (ELSEVIER)S0169-555X(20)30559-6 DE-627 ger DE-627 rakwb eng 650 VZ Li, Zhihai verfasserin aut Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway 2021transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Wang, Qing oth Zhou, Fujun oth Li, Yuchao oth Han, Xudong oth Mehmood, Qaiser oth Cao, Chen oth Gu, FeiFan oth Han, Mengxia oth Chen, Jianping oth Enthalten in Elsevier Science Paltrinieri, Andrea ELSEVIER Islamic finance development and banking ESG scores: Evidence from a cross-country analysis 2019 Amsterdam [u.a.] (DE-627)ELV003279995 volume:377 year:2021 day:15 month:03 pages:0 https://doi.org/10.1016/j.geomorph.2020.107586 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U AR 377 2021 15 0315 0 |
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10.1016/j.geomorph.2020.107586 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001299.pica (DE-627)ELV053105982 (ELSEVIER)S0169-555X(20)30559-6 DE-627 ger DE-627 rakwb eng 650 VZ Li, Zhihai verfasserin aut Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway 2021transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Wang, Qing oth Zhou, Fujun oth Li, Yuchao oth Han, Xudong oth Mehmood, Qaiser oth Cao, Chen oth Gu, FeiFan oth Han, Mengxia oth Chen, Jianping oth Enthalten in Elsevier Science Paltrinieri, Andrea ELSEVIER Islamic finance development and banking ESG scores: Evidence from a cross-country analysis 2019 Amsterdam [u.a.] (DE-627)ELV003279995 volume:377 year:2021 day:15 month:03 pages:0 https://doi.org/10.1016/j.geomorph.2020.107586 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U AR 377 2021 15 0315 0 |
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10.1016/j.geomorph.2020.107586 doi /cbs_pica/cbs_olc/import_discovery/elsevier/einzuspielen/GBV00000000001299.pica (DE-627)ELV053105982 (ELSEVIER)S0169-555X(20)30559-6 DE-627 ger DE-627 rakwb eng 650 VZ Li, Zhihai verfasserin aut Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway 2021transfer abstract nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. Wang, Qing oth Zhou, Fujun oth Li, Yuchao oth Han, Xudong oth Mehmood, Qaiser oth Cao, Chen oth Gu, FeiFan oth Han, Mengxia oth Chen, Jianping oth Enthalten in Elsevier Science Paltrinieri, Andrea ELSEVIER Islamic finance development and banking ESG scores: Evidence from a cross-country analysis 2019 Amsterdam [u.a.] (DE-627)ELV003279995 volume:377 year:2021 day:15 month:03 pages:0 https://doi.org/10.1016/j.geomorph.2020.107586 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U AR 377 2021 15 0315 0 |
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integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the tongmai old deposit along the sichuan-tibet railway |
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Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway |
| abstract |
Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. |
| abstractGer |
Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. |
| abstract_unstemmed |
Numerous old deposits occur in the Eastern Himalayan Syntaxis, especially on the banks of the Yarlung Tsangpo River and its tributaries, where strong tectonic movement and riverine erosion increase the potential for landslides. The possible future deformation and failure processes of these old deposits and their impacts on the surrounding environment are important research topics. Field investigations and temporarily coherent point interferometry synthetic aperture radar (TCP-InSAR) monitoring show that the Tongmai old deposit is prone to catastrophic failure and landsliding. A geomorphological analysis and the related dating results indicate that the Tongmai old deposit consists of residual colluvial or early moraine debris and was formed later than 11.06 ± 0.94 ka BP. The TCP-InSAR analysis indicates that creep deformation is present within the deposit and that this creep is closely related to the precipitation and activity of nearby faults, which may cause slope failure and lead to landslide dam formation. As a result, this study further predicts the likely scale of a landslide dam through numerical simulations. In the worst-case scenario, a landslide will seriously block the Parlung Tsangpo River and form a dam with a height of 100–152 m and a length of approximately 2.4 km. The Tongmai old deposit will likely form a geohazard chain including landslides, barrier lakes, and outburst flooding. Finally, this paper discusses the influence of the Tongmai old deposit on river and landscape evolution. |
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Integrating an interferometric synthetic aperture radar technique and numerical simulation to investigate the Tongmai old deposit along the Sichuan-Tibet Railway |
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