Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures
Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conduct...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Liang, Xiaofeng [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© Science China Press 2023 |
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| Übergeordnetes Werk: |
Enthalten in: Science in China - Heidelberg : Springer, 1997, 66(2023), 12 vom: 02. Nov., Seite 2770-2790 |
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| Übergeordnetes Werk: |
volume:66 ; year:2023 ; number:12 ; day:02 ; month:11 ; pages:2770-2790 |
| Links: |
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| DOI / URN: |
10.1007/s11430-023-1158-5 |
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| 520 | |a Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. | ||
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10.1007/s11430-023-1158-5 doi (DE-627)SPR053989139 (SPR)s11430-023-1158-5-e DE-627 ger DE-627 rakwb eng Liang, Xiaofeng verfasserin aut Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science China Press 2023 Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 Chen, Ling aut Tian, Xiaobo aut Chu, Yang aut Li, Wentao aut Enthalten in Science in China Heidelberg : Springer, 1997 66(2023), 12 vom: 02. Nov., Seite 2770-2790 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:66 year:2023 number:12 day:02 month:11 pages:2770-2790 https://dx.doi.org/10.1007/s11430-023-1158-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 66 2023 12 02 11 2770-2790 |
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10.1007/s11430-023-1158-5 doi (DE-627)SPR053989139 (SPR)s11430-023-1158-5-e DE-627 ger DE-627 rakwb eng Liang, Xiaofeng verfasserin aut Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science China Press 2023 Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 Chen, Ling aut Tian, Xiaobo aut Chu, Yang aut Li, Wentao aut Enthalten in Science in China Heidelberg : Springer, 1997 66(2023), 12 vom: 02. Nov., Seite 2770-2790 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:66 year:2023 number:12 day:02 month:11 pages:2770-2790 https://dx.doi.org/10.1007/s11430-023-1158-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 66 2023 12 02 11 2770-2790 |
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10.1007/s11430-023-1158-5 doi (DE-627)SPR053989139 (SPR)s11430-023-1158-5-e DE-627 ger DE-627 rakwb eng Liang, Xiaofeng verfasserin aut Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science China Press 2023 Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 Chen, Ling aut Tian, Xiaobo aut Chu, Yang aut Li, Wentao aut Enthalten in Science in China Heidelberg : Springer, 1997 66(2023), 12 vom: 02. Nov., Seite 2770-2790 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:66 year:2023 number:12 day:02 month:11 pages:2770-2790 https://dx.doi.org/10.1007/s11430-023-1158-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 66 2023 12 02 11 2770-2790 |
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10.1007/s11430-023-1158-5 doi (DE-627)SPR053989139 (SPR)s11430-023-1158-5-e DE-627 ger DE-627 rakwb eng Liang, Xiaofeng verfasserin aut Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science China Press 2023 Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 Chen, Ling aut Tian, Xiaobo aut Chu, Yang aut Li, Wentao aut Enthalten in Science in China Heidelberg : Springer, 1997 66(2023), 12 vom: 02. Nov., Seite 2770-2790 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:66 year:2023 number:12 day:02 month:11 pages:2770-2790 https://dx.doi.org/10.1007/s11430-023-1158-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 66 2023 12 02 11 2770-2790 |
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10.1007/s11430-023-1158-5 doi (DE-627)SPR053989139 (SPR)s11430-023-1158-5-e DE-627 ger DE-627 rakwb eng Liang, Xiaofeng verfasserin aut Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Science China Press 2023 Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 Chen, Ling aut Tian, Xiaobo aut Chu, Yang aut Li, Wentao aut Enthalten in Science in China Heidelberg : Springer, 1997 66(2023), 12 vom: 02. Nov., Seite 2770-2790 (DE-627)385614748 (DE-600)2142896-7 1862-2801 nnns volume:66 year:2023 number:12 day:02 month:11 pages:2770-2790 https://dx.doi.org/10.1007/s11430-023-1158-5 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 AR 66 2023 12 02 11 2770-2790 |
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Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures Tibetan Plateau (dpeaa)DE-He213 Crustal structure (dpeaa)DE-He213 Moho doublet (dpeaa)DE-He213 Uplift of the plateau (dpeaa)DE-He213 Crustal channel flow (dpeaa)DE-He213 |
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uplifting mechanism of the tibetan plateau inferred from the characteristics of crustal structures |
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Uplifting mechanism of the Tibetan Plateau inferred from the characteristics of crustal structures |
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Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. © Science China Press 2023 |
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Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. © Science China Press 2023 |
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Abstract The Tibetan Plateau has been known for its highest elevation and thickest crust on earth, and become a key region for comprehending the rheology and tectonic evolution of continental plates and associated dynamic processes. Over the past years, numerous geophysical studies have been conducted to explore the deep structure of the Tibetan Plateau, resulting in significant advancements in understanding the formation and growth of the Plateau. This paper aims to provide a comprehensive summary and discussion of the geophysical observations and underlying mechanisms of the plateau uplift. First, major relevant tectonic models are reviewed, and the corresponding features of crustal structures and related deformation are presented. Then, recent observations, including the identification of a high-velocity layer in the lower crust of the Lhasa block, the spatial distribution of crustal channel flow, and the decoupling of shallow and deep crustal deformation, are synthesized to gain insights into the crustal structures, and multidisciplinary data are integrated to discuss the potential mechanisms of the plateau uplift. Lastly, some pertinent suggestions are put forward for future research on the Tibetan Plateau. © Science China Press 2023 |
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