Matches in SemOpenAlex for { <https://semopenalex.org/work/W3049447500> ?p ?o ?g. }
- W3049447500 endingPage "107373" @default.
- W3049447500 startingPage "107373" @default.
- W3049447500 abstract "Abstract The study of drainage evolution in the Songnen Plain, Northeast China, is essential for understanding the interactions between tectonics-topography-climate-drainage evolution in the region. Despite this, it remains unclear whether the paleo-Songhua River (upper-middle reaches of the Songhua River) once flowed westward into the Songnen Plain and what forcings influenced the drainage development of the Songnen Plain. In this contribution, we provide insight into drainage development on the Songnen Plain using an integrated approach of magnetic susceptibility, geochemical (elemental and Sr Nd isotopic) and heavy mineral composition recovered from a 102-m sediment core sediments extracted from the eastern edge of the Songnen Plain with sedimentological and topographic archives. Our results show that a dramatic provenance shift occurred at the depth of 62.2 m (~0.94 Ma) in the core sediments. It is proposed that the Songhua River was separated by the Jia-Yi (Jiamushi-Yilan) divide into two segments before ~0.94 Ma, the west-flowing proto-Songhua River and the east-flowing proto-Sanjiang River (lower reach of the Songhua River). However, the proto-Songhua River reversed direction at ~0.94 Ma when the Jia-Yi divide was cut through by headward erosion of the proto-Sanjiang River, marking the birth of the Songhua River as a single, eastward-flowing river system. Tectonics is suggested as the first-order control on the evolution of the Songhua River before 1.20 Ma, whereas climate changes may be responsible after 1.20 Ma." @default.
- W3049447500 created "2020-08-21" @default.
- W3049447500 creator A5011967355 @default.
- W3049447500 creator A5025590856 @default.
- W3049447500 creator A5026706337 @default.
- W3049447500 creator A5030042849 @default.
- W3049447500 creator A5032597713 @default.
- W3049447500 creator A5036949743 @default.
- W3049447500 creator A5049625251 @default.
- W3049447500 date "2020-11-01" @default.
- W3049447500 modified "2023-10-17" @default.
- W3049447500 title "Reversal of the middle-upper Songhua River in the late Early Pleistocene, Northeast China" @default.
- W3049447500 cites W1529031231 @default.
- W3049447500 cites W1543840266 @default.
- W3049447500 cites W1965701586 @default.
- W3049447500 cites W1981662873 @default.
- W3049447500 cites W1983602215 @default.
- W3049447500 cites W1984696539 @default.
- W3049447500 cites W1988627424 @default.
- W3049447500 cites W1989574467 @default.
- W3049447500 cites W1995028274 @default.
- W3049447500 cites W1998670404 @default.
- W3049447500 cites W1998750657 @default.
- W3049447500 cites W2000077199 @default.
- W3049447500 cites W2003767587 @default.
- W3049447500 cites W2003909939 @default.
- W3049447500 cites W2007852823 @default.
- W3049447500 cites W2016372936 @default.
- W3049447500 cites W2019558782 @default.
- W3049447500 cites W2020551982 @default.
- W3049447500 cites W2024136445 @default.
- W3049447500 cites W2024698368 @default.
- W3049447500 cites W2027769899 @default.
- W3049447500 cites W2029401070 @default.
- W3049447500 cites W2029945405 @default.
- W3049447500 cites W2031171042 @default.
- W3049447500 cites W2031461723 @default.
- W3049447500 cites W2032078206 @default.
- W3049447500 cites W2036434409 @default.
- W3049447500 cites W2038300170 @default.
- W3049447500 cites W2040236851 @default.
- W3049447500 cites W2047168195 @default.
- W3049447500 cites W2049561582 @default.
- W3049447500 cites W2050716036 @default.
- W3049447500 cites W2054153880 @default.
- W3049447500 cites W2062797763 @default.
- W3049447500 cites W2063254743 @default.
- W3049447500 cites W2076170666 @default.
- W3049447500 cites W2079900432 @default.
- W3049447500 cites W2084378009 @default.
- W3049447500 cites W2088323032 @default.
- W3049447500 cites W2089284596 @default.
- W3049447500 cites W2090240681 @default.
- W3049447500 cites W2095118773 @default.
- W3049447500 cites W2102372757 @default.
- W3049447500 cites W2102832616 @default.
- W3049447500 cites W2104224684 @default.
- W3049447500 cites W2108316127 @default.
- W3049447500 cites W2118204502 @default.
- W3049447500 cites W2125510776 @default.
- W3049447500 cites W2153038124 @default.
- W3049447500 cites W2158324412 @default.
- W3049447500 cites W2162898351 @default.
- W3049447500 cites W2261283149 @default.
- W3049447500 cites W2302516385 @default.
- W3049447500 cites W2512748803 @default.
- W3049447500 cites W2560257251 @default.
- W3049447500 cites W2568995328 @default.
- W3049447500 cites W2572639775 @default.
- W3049447500 cites W2593929300 @default.
- W3049447500 cites W2593999116 @default.
- W3049447500 cites W2741367689 @default.
- W3049447500 cites W2748330772 @default.
- W3049447500 cites W2760384334 @default.
- W3049447500 cites W2771289517 @default.
- W3049447500 cites W2772821439 @default.
- W3049447500 cites W2775002788 @default.
- W3049447500 cites W2778912433 @default.
- W3049447500 cites W2885973884 @default.
- W3049447500 cites W2892199940 @default.
- W3049447500 cites W2897861431 @default.
- W3049447500 cites W2949291400 @default.
- W3049447500 cites W2949873343 @default.
- W3049447500 cites W2954881943 @default.
- W3049447500 cites W2964931786 @default.
- W3049447500 cites W2978834555 @default.
- W3049447500 cites W2981230410 @default.
- W3049447500 cites W2988801126 @default.
- W3049447500 cites W3018483315 @default.
- W3049447500 cites W3040368166 @default.
- W3049447500 cites W4238778566 @default.
- W3049447500 cites W796896008 @default.
- W3049447500 doi "https://doi.org/10.1016/j.geomorph.2020.107373" @default.
- W3049447500 hasPublicationYear "2020" @default.
- W3049447500 type Work @default.
- W3049447500 sameAs 3049447500 @default.
- W3049447500 citedByCount "8" @default.
- W3049447500 countsByYear W30494475002021 @default.