Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift

Along the lower reaches of the Yarlung Zangbo River, scattered alluvium sections appear on T1 and T2 terraces. The alluvial deposits on the T1 terrace in Linduo and Ximogou and the T2 terrace in Guoguotang are composed principally of coarse-grained sand particles and rock fragments, with no observab...

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Main Authors: Xie Chao, Zhou Bengang, Li Zhengfang, Yang Fan, Pang Wei, Li Wei
Format: Article
Language:English
Published: De Gruyter 2020-12-01
Series:Open Geosciences
Subjects:
Online Access:https://doi.org/10.1515/geo-2020-0215
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spelling doaj-d8f69aba64e04cc38b47d761425f96bb2021-09-05T20:50:52ZengDe GruyterOpen Geosciences2391-54472020-12-011211645165210.1515/geo-2020-0215geo-2020-0215Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic upliftXie Chao0Zhou Bengang1Li Zhengfang2Yang Fan3Pang Wei4Li Wei5The Institute of Crust Movement and Hazard Risk, The Second Monitoring and Application Center, China Earthquake Administration, Xi’an, Shaanxi, 710054, ChinaKey Laboratory of Seismic and Volcanic Hazards, China Earthquake Administration, Beijing, 100029, ChinaKey Laboratory of Seismic and Volcanic Hazards, China Earthquake Administration, Beijing, 100029, ChinaThe Institute of Crust Movement and Hazard Risk, The Second Monitoring and Application Center, China Earthquake Administration, Xi’an, Shaanxi, 710054, ChinaThe Institute of Crust Movement and Hazard Risk, The Second Monitoring and Application Center, China Earthquake Administration, Xi’an, Shaanxi, 710054, ChinaThe Institute of Crust Movement and Hazard Risk, The Second Monitoring and Application Center, China Earthquake Administration, Xi’an, Shaanxi, 710054, ChinaAlong the lower reaches of the Yarlung Zangbo River, scattered alluvium sections appear on T1 and T2 terraces. The alluvial deposits on the T1 terrace in Linduo and Ximogou and the T2 terrace in Guoguotang are composed principally of coarse-grained sand particles and rock fragments, with no observable fine-grained components. The T1 terrace alluvium section is dominated by clay and silt and occurs near the town of Dexing, and optically stimulated luminescence dating of sample from this site revealed an age of 18.2 kyear, which indicates that the incision rate of the Yarlung Zangbo River has been 4.7 mm/year since the formation of this section. On the basis of the component characteristics of terraces in Motuo County, the provenance for the terraces is probably related to the breaking of the palaeo-dammed lakes in the middle reaches of the Yarlung Zangbo River. A 430 m elevation difference still exists between the study area and the local base level downstream of the Yalung Zangbo River (Assam Plain), although this river has a strong incision capability (4.7 mm/year), which suggests that tectonic uplift remains very intense east of the Namche Barwa syntaxis.https://doi.org/10.1515/geo-2020-0215lower reaches of the yarlung zangbo riverterraceoptically stimulated luminescence ageincision ratetectonic uplift
collection DOAJ
language English
format Article
sources DOAJ
author Xie Chao
Zhou Bengang
Li Zhengfang
Yang Fan
Pang Wei
Li Wei
spellingShingle Xie Chao
Zhou Bengang
Li Zhengfang
Yang Fan
Pang Wei
Li Wei
Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
Open Geosciences
lower reaches of the yarlung zangbo river
terrace
optically stimulated luminescence age
incision rate
tectonic uplift
author_facet Xie Chao
Zhou Bengang
Li Zhengfang
Yang Fan
Pang Wei
Li Wei
author_sort Xie Chao
title Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
title_short Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
title_full Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
title_fullStr Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
title_full_unstemmed Features of terraces and the incision rate along the lower reaches of the Yarlung Zangbo River east of Namche Barwa: Constraints on tectonic uplift
title_sort features of terraces and the incision rate along the lower reaches of the yarlung zangbo river east of namche barwa: constraints on tectonic uplift
publisher De Gruyter
series Open Geosciences
issn 2391-5447
publishDate 2020-12-01
description Along the lower reaches of the Yarlung Zangbo River, scattered alluvium sections appear on T1 and T2 terraces. The alluvial deposits on the T1 terrace in Linduo and Ximogou and the T2 terrace in Guoguotang are composed principally of coarse-grained sand particles and rock fragments, with no observable fine-grained components. The T1 terrace alluvium section is dominated by clay and silt and occurs near the town of Dexing, and optically stimulated luminescence dating of sample from this site revealed an age of 18.2 kyear, which indicates that the incision rate of the Yarlung Zangbo River has been 4.7 mm/year since the formation of this section. On the basis of the component characteristics of terraces in Motuo County, the provenance for the terraces is probably related to the breaking of the palaeo-dammed lakes in the middle reaches of the Yarlung Zangbo River. A 430 m elevation difference still exists between the study area and the local base level downstream of the Yalung Zangbo River (Assam Plain), although this river has a strong incision capability (4.7 mm/year), which suggests that tectonic uplift remains very intense east of the Namche Barwa syntaxis.
topic lower reaches of the yarlung zangbo river
terrace
optically stimulated luminescence age
incision rate
tectonic uplift
url https://doi.org/10.1515/geo-2020-0215
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