Matches in SemOpenAlex for { <https://semopenalex.org/work/W3007454787> ?p ?o ?g. }
- W3007454787 endingPage "107100" @default.
- W3007454787 startingPage "107100" @default.
- W3007454787 abstract "River-incision rate is widely used to track changes in tectonics or climate over time and space. However, the feasibility of utilizing the spatial variations of river incision to reconstruct past tectonic and climatic processes remains unclear. Here, we focus on the spatial patterns of river incision along the northern Chinese Tian Shan foreland. Three alluvial fans FP, FeH, and FlH are determined as the alluvial fan context of river incision and terrace classification providing the geomorphological framework across the foreland region. Four rivers (i.e. the Kuitun, Jingou, Manas, and Urumqi Rivers from the western, central, and eastern part of the foreland) are used to reconstruct the paleogeomorphology from the reference, which is the best-preserved terrace of each river system with ages clustering in different parts of the Latest Pleistocene-Early Holocene. The depth of incision constrained by the reference terrace of each river is obtained by comparing the present-day topography and the reconstructed one. The resulting profile of channel incision (depth and rate) of each analyzed river displays an overall decreasing-downstream trend from the maximum where the river exits from the mountain range, to zero. Such a trend has been attributed to the progressive lowering of the river gradient that was caused by the adjusted ratio of sediment input versus water discharge induced by climate change. Superimposing on the decreasing-downstream trend, an obvious step can also easily be observed onto the profile of channel incision of each river, downstream of which channel incision is significantly less. The step occurs near the thrust fault controlling growth of the outermost anticline through which each river cuts, thereby implying the key role of local rock uplift in forming the river-incision step. The former observation implies that, at the same timescale, more river incision at the exit from the mountain range does not necessarily mean stronger climatic forcing of incision there. We thus propose that, in a foreland setting, it should be the temporal pattern of river incision rather than its spatial variation that is helpful for unraveling the change in the forcing factor of downcutting." @default.
- W3007454787 created "2020-03-06" @default.
- W3007454787 creator A5002218979 @default.
- W3007454787 creator A5021343257 @default.
- W3007454787 creator A5027827976 @default.
- W3007454787 creator A5032956501 @default.
- W3007454787 creator A5065346153 @default.
- W3007454787 creator A5091712868 @default.
- W3007454787 date "2020-05-01" @default.
- W3007454787 modified "2023-10-17" @default.
- W3007454787 title "Spatial patterns of Late Quaternary river incision along the northern Tian Shan foreland" @default.
- W3007454787 cites W1631559605 @default.
- W3007454787 cites W1635932458 @default.
- W3007454787 cites W1921450070 @default.
- W3007454787 cites W1966903975 @default.
- W3007454787 cites W1975821545 @default.
- W3007454787 cites W1987316269 @default.
- W3007454787 cites W1999730394 @default.
- W3007454787 cites W2004752263 @default.
- W3007454787 cites W2006536407 @default.
- W3007454787 cites W2008834035 @default.
- W3007454787 cites W2009289957 @default.
- W3007454787 cites W2011455121 @default.
- W3007454787 cites W2013651167 @default.
- W3007454787 cites W2013686379 @default.
- W3007454787 cites W2014440168 @default.
- W3007454787 cites W2014997517 @default.
- W3007454787 cites W2015673335 @default.
- W3007454787 cites W2015984263 @default.
- W3007454787 cites W2017596128 @default.
- W3007454787 cites W2017814036 @default.
- W3007454787 cites W2028528785 @default.
- W3007454787 cites W2036894547 @default.
- W3007454787 cites W2041806930 @default.
- W3007454787 cites W2051992811 @default.
- W3007454787 cites W2059054619 @default.
- W3007454787 cites W2071604291 @default.
- W3007454787 cites W2081265741 @default.
- W3007454787 cites W2090756337 @default.
- W3007454787 cites W2095079131 @default.
- W3007454787 cites W2104300819 @default.
- W3007454787 cites W2111204986 @default.
- W3007454787 cites W2120286752 @default.
- W3007454787 cites W2123793538 @default.
- W3007454787 cites W2128393314 @default.
- W3007454787 cites W2140403093 @default.
- W3007454787 cites W2140726382 @default.
- W3007454787 cites W2146516853 @default.
- W3007454787 cites W2148162674 @default.
- W3007454787 cites W2149342649 @default.
- W3007454787 cites W2149866460 @default.
- W3007454787 cites W2154684728 @default.
- W3007454787 cites W2161057903 @default.
- W3007454787 cites W2162429799 @default.
- W3007454787 cites W2171598953 @default.
- W3007454787 cites W2202435839 @default.
- W3007454787 cites W2228325661 @default.
- W3007454787 cites W2258790957 @default.
- W3007454787 cites W2329443912 @default.
- W3007454787 cites W2380818311 @default.
- W3007454787 cites W2494000845 @default.
- W3007454787 cites W2528686645 @default.
- W3007454787 cites W2534025652 @default.
- W3007454787 cites W2535709166 @default.
- W3007454787 cites W2542511845 @default.
- W3007454787 cites W2554046248 @default.
- W3007454787 cites W2573359620 @default.
- W3007454787 cites W2612149827 @default.
- W3007454787 cites W2617663108 @default.
- W3007454787 cites W2735169904 @default.
- W3007454787 cites W2758608764 @default.
- W3007454787 cites W2766279044 @default.
- W3007454787 cites W2767598057 @default.
- W3007454787 cites W2783750832 @default.
- W3007454787 cites W2789294083 @default.
- W3007454787 cites W2806114501 @default.
- W3007454787 cites W2807847095 @default.
- W3007454787 cites W2897861431 @default.
- W3007454787 cites W2943351852 @default.
- W3007454787 cites W2982051580 @default.
- W3007454787 cites W638029671 @default.
- W3007454787 doi "https://doi.org/10.1016/j.geomorph.2020.107100" @default.
- W3007454787 hasPublicationYear "2020" @default.
- W3007454787 type Work @default.
- W3007454787 sameAs 3007454787 @default.
- W3007454787 citedByCount "13" @default.
- W3007454787 countsByYear W30074547872021 @default.
- W3007454787 countsByYear W30074547872022 @default.
- W3007454787 countsByYear W30074547872023 @default.
- W3007454787 crossrefType "journal-article" @default.
- W3007454787 hasAuthorship W3007454787A5002218979 @default.
- W3007454787 hasAuthorship W3007454787A5021343257 @default.
- W3007454787 hasAuthorship W3007454787A5027827976 @default.
- W3007454787 hasAuthorship W3007454787A5032956501 @default.
- W3007454787 hasAuthorship W3007454787A5065346153 @default.
- W3007454787 hasAuthorship W3007454787A5091712868 @default.
- W3007454787 hasConcept C109007969 @default.
- W3007454787 hasConcept C114793014 @default.