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• W3023956435 endingPage "107213" @default.
• W3023956435 startingPage "107213" @default.
• W3023956435 abstract "Abstract The Yulin River in the northern Tibetan Plateau, consists of multiple geomorphological features, including alluvial fans, fluvial terraces, and river profile knickpoints. Collectively, these provide a natural laboratory for exploring the late Quaternary fluvial landform evolution in response to both climatic change and tectonic activities in the region of the Altyn Tagh Fault. In this study, we investigated the distribution, sequences and sediment characteristics of the fluvial landforms along the Yulin River based on high-precision (0.5 m-resolution) Worldview satellite images and field observations. Mid-Pleistocene alluvial fans formed the highest fluvial landform surface into which ten major inset fluvial terraces were developed, distributed along three stream segments. Real-time kinematic global positioning system (RTK-GPS) measurement of terrace surfaces and the modern river longitudinal profiles was conducted across the Dongbatu Shan to show fluvial landform geometry and tectonic deformation. Fluvial terrace surfaces were deformed due to fault uplift as illustrated by spatially variable surface geometries. The chronological sequences of terraces along the Yulin River since 160 ka were reconstructed based on 10Be terrestrial cosmogenic nuclides (TCNs) dating. Results indicated that river incision occurred mainly during periods of climate transition, suggesting that terrace evolution was partly controlled by climate changes. Moreover, terrace exposure ages showed an upstream younging trend along the river, demonstrating a probable response to knickpoint retreat. Combined with terrace deformation and ages, fault uplift rates were constrained, which were lower than the river incision rates during the Late Quaternary, indicating that crustal shortening was mainly absorbed by the growth of the regional anticline. Collectively, our results suggest that the evolution of fluvial landforms along the Yulin River is a function of interplay between regional tectonic activities and climatic changes, which is significant to understand the NW-outward splay of the Altyn Tagh Fault." @default.
• W3023956435 created "2020-05-13" @default.
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• W3023956435 date "2020-08-01" @default.
• W3023956435 modified "2023-10-13" @default.
• W3023956435 title "Late Quaternary fluvial landform evolution and controlling factors along the Yulin River on the Northern Tibetan Plateau" @default.
• W3023956435 cites W1077071167 @default.
• W3023956435 cites W1526822975 @default.
• W3023956435 cites W1565431790 @default.
• W3023956435 cites W1592988921 @default.
• W3023956435 cites W1647644057 @default.
• W3023956435 cites W1872453959 @default.
• W3023956435 cites W1920894272 @default.
• W3023956435 cites W1946046604 @default.
• W3023956435 cites W1965098282 @default.
• W3023956435 cites W1965273505 @default.
• W3023956435 cites W1967502633 @default.
• W3023956435 cites W1975350041 @default.
• W3023956435 cites W1976822911 @default.
• W3023956435 cites W1990375499 @default.
• W3023956435 cites W1995235969 @default.
• W3023956435 cites W1995947668 @default.
• W3023956435 cites W1996923801 @default.
• W3023956435 cites W1998456714 @default.
• W3023956435 cites W2002325302 @default.
• W3023956435 cites W2002473398 @default.
• W3023956435 cites W2005035365 @default.
• W3023956435 cites W2006536407 @default.
• W3023956435 cites W2007273878 @default.
• W3023956435 cites W2008834035 @default.
• W3023956435 cites W2008875043 @default.
• W3023956435 cites W2009425598 @default.
• W3023956435 cites W2010455802 @default.
• W3023956435 cites W2014440168 @default.
• W3023956435 cites W2016138287 @default.
• W3023956435 cites W2018502726 @default.
• W3023956435 cites W2019504758 @default.
• W3023956435 cites W2021434403 @default.
• W3023956435 cites W2022422776 @default.
• W3023956435 cites W2024181735 @default.
• W3023956435 cites W2025127191 @default.
• W3023956435 cites W2026072617 @default.
• W3023956435 cites W2027135620 @default.
• W3023956435 cites W2031131776 @default.
• W3023956435 cites W2035413487 @default.
• W3023956435 cites W2036894547 @default.
• W3023956435 cites W2040511317 @default.
• W3023956435 cites W2041774199 @default.
• W3023956435 cites W2044945380 @default.
• W3023956435 cites W2053523315 @default.
• W3023956435 cites W2056084716 @default.
• W3023956435 cites W2063155650 @default.
• W3023956435 cites W2064009645 @default.
• W3023956435 cites W2064066626 @default.
• W3023956435 cites W2068270668 @default.
• W3023956435 cites W2068985200 @default.
• W3023956435 cites W2071237400 @default.
• W3023956435 cites W2071511432 @default.
• W3023956435 cites W2072716553 @default.
• W3023956435 cites W2076170666 @default.
• W3023956435 cites W2081357941 @default.
• W3023956435 cites W2089284596 @default.
• W3023956435 cites W2094475308 @default.
• W3023956435 cites W2099265637 @default.
• W3023956435 cites W2106101192 @default.
• W3023956435 cites W2109287321 @default.
• W3023956435 cites W2109948872 @default.
• W3023956435 cites W2110321124 @default.
• W3023956435 cites W2111151668 @default.
• W3023956435 cites W2112815562 @default.
• W3023956435 cites W2118381748 @default.
• W3023956435 cites W2119723973 @default.
• W3023956435 cites W2120748836 @default.
• W3023956435 cites W2124538525 @default.
• W3023956435 cites W2127335932 @default.
• W3023956435 cites W2129102590 @default.
• W3023956435 cites W2130615188 @default.
• W3023956435 cites W2130994975 @default.
• W3023956435 cites W2147429383 @default.
• W3023956435 cites W2155880045 @default.
• W3023956435 cites W2180911899 @default.
• W3023956435 cites W2265024238 @default.
• W3023956435 cites W2314299591 @default.
• W3023956435 cites W2329027129 @default.
• W3023956435 cites W2380818311 @default.
• W3023956435 cites W2508524488 @default.
• W3023956435 cites W2529727159 @default.
• W3023956435 cites W2535709166 @default.
• W3023956435 cites W2560205414 @default.
• W3023956435 cites W2564693580 @default.

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