Matches in SemOpenAlex for { <https://semopenalex.org/work/W2998513828> ?p ?o ?g. }
- W2998513828 endingPage "104224" @default.
- W2998513828 startingPage "104224" @default.
- W2998513828 abstract "Fluvial terraces are common in the tectonically active western Kunlun Mountains (WKLM) region, northwestern margin of the Tibetan Plateau, and incision of rivers since 5 ka was attributed to the accelerated uplift of the WKLM. However, it is difficult to evaluate their tectonic or climatic origin without detailed chronology. In this study, Optically Stimulated Luminescence (OSL) dating was applied to fluvial/flood and aeolian sediments on five lowest fluvial terraces (49 m in total) along the Keriya River, and the 21 OSL ages (from 11 samples) revealed the incision processes since the mid-Holocene, especially the fast incision (3.5–0 ka, 10.9 mm/a) during the late Holocene. This was supported by the climatic background, i.e., increased precipitation from the westerlies and meltwater from frequent glacial advance-retreat events. As a response to the climatic changes, large-scale floods were frequent as well, e.g., at 3.5, 2.6, 0.87, and 0.25 ka, which were crucial for the fast incisions on the filling gravels. Additionally, the flood also caused the river’s further extension into the Taklamakan Desert and controlled the evolution of oases in the desert, including ancient cities and cultures. Consequently, we suggest that climatic change was important for the incision and formation of cut-in-fill terraces along the Keriya River during the Holocene, and influences from other factors, including surface uplift, should not be ignored, but were difficult to be evaluated." @default.
- W2998513828 created "2020-01-10" @default.
- W2998513828 creator A5029437844 @default.
- W2998513828 creator A5031944678 @default.
- W2998513828 creator A5034745329 @default.
- W2998513828 creator A5035655272 @default.
- W2998513828 creator A5047374324 @default.
- W2998513828 creator A5061816710 @default.
- W2998513828 creator A5067702320 @default.
- W2998513828 date "2020-04-01" @default.
- W2998513828 modified "2023-10-15" @default.
- W2998513828 title "Holocene incisions and flood activities of the Keriya River, NW margin of the Tibetan plateau" @default.
- W2998513828 cites W1544329654 @default.
- W2998513828 cites W1774412088 @default.
- W2998513828 cites W1971074221 @default.
- W2998513828 cites W1975052733 @default.
- W2998513828 cites W1977225883 @default.
- W2998513828 cites W1982602424 @default.
- W2998513828 cites W1985036125 @default.
- W2998513828 cites W1986082054 @default.
- W2998513828 cites W1990899433 @default.
- W2998513828 cites W1992317256 @default.
- W2998513828 cites W1995521250 @default.
- W2998513828 cites W1995672440 @default.
- W2998513828 cites W1996932107 @default.
- W2998513828 cites W2001938821 @default.
- W2998513828 cites W2006144783 @default.
- W2998513828 cites W2011221215 @default.
- W2998513828 cites W2013878295 @default.
- W2998513828 cites W2018238674 @default.
- W2998513828 cites W2020551982 @default.
- W2998513828 cites W2021672970 @default.
- W2998513828 cites W2024871471 @default.
- W2998513828 cites W2025127191 @default.
- W2998513828 cites W2034034969 @default.
- W2998513828 cites W2036205938 @default.
- W2998513828 cites W2036581996 @default.
- W2998513828 cites W2038068461 @default.
- W2998513828 cites W2042219694 @default.
- W2998513828 cites W2044319030 @default.
- W2998513828 cites W2046061916 @default.
- W2998513828 cites W2046587735 @default.
- W2998513828 cites W2049422652 @default.
- W2998513828 cites W2050585743 @default.
- W2998513828 cites W2052493774 @default.
- W2998513828 cites W2058060439 @default.
- W2998513828 cites W2067643634 @default.
- W2998513828 cites W2077375337 @default.
- W2998513828 cites W2077784993 @default.
- W2998513828 cites W2084794993 @default.
- W2998513828 cites W2094408279 @default.
- W2998513828 cites W2104344570 @default.
- W2998513828 cites W2104754642 @default.
- W2998513828 cites W2109269291 @default.
- W2998513828 cites W2110418145 @default.
- W2998513828 cites W2136718048 @default.
- W2998513828 cites W2145035874 @default.
- W2998513828 cites W2147429383 @default.
- W2998513828 cites W2147601362 @default.
- W2998513828 cites W2151563885 @default.
- W2998513828 cites W2154684728 @default.
- W2998513828 cites W2164982993 @default.
- W2998513828 cites W2207495354 @default.
- W2998513828 cites W2289328486 @default.
- W2998513828 cites W2326956302 @default.
- W2998513828 cites W2473752769 @default.
- W2998513828 cites W2587961719 @default.
- W2998513828 cites W2607203176 @default.
- W2998513828 cites W2766279044 @default.
- W2998513828 cites W2767068729 @default.
- W2998513828 cites W2790059128 @default.
- W2998513828 cites W2800495832 @default.
- W2998513828 cites W2803674428 @default.
- W2998513828 cites W2884967374 @default.
- W2998513828 cites W2892199940 @default.
- W2998513828 cites W2895578688 @default.
- W2998513828 cites W2921069043 @default.
- W2998513828 cites W2952274226 @default.
- W2998513828 cites W4232236196 @default.
- W2998513828 doi "https://doi.org/10.1016/j.jseaes.2019.104224" @default.
- W2998513828 hasPublicationYear "2020" @default.
- W2998513828 type Work @default.
- W2998513828 sameAs 2998513828 @default.
- W2998513828 citedByCount "11" @default.
- W2998513828 countsByYear W29985138282021 @default.
- W2998513828 countsByYear W29985138282022 @default.
- W2998513828 countsByYear W29985138282023 @default.
- W2998513828 crossrefType "journal-article" @default.
- W2998513828 hasAuthorship W2998513828A5029437844 @default.
- W2998513828 hasAuthorship W2998513828A5031944678 @default.
- W2998513828 hasAuthorship W2998513828A5034745329 @default.
- W2998513828 hasAuthorship W2998513828A5035655272 @default.
- W2998513828 hasAuthorship W2998513828A5047374324 @default.
- W2998513828 hasAuthorship W2998513828A5061816710 @default.
- W2998513828 hasAuthorship W2998513828A5067702320 @default.
- W2998513828 hasConcept C100970517 @default.
- W2998513828 hasConcept C109007969 @default.
- W2998513828 hasConcept C111368507 @default.