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- W2901403746 abstract "Abstract Overbank deposits in the Komissarovka River valley consist of alternating silt, clay silt, sand, and soils produced by lacustrine, alluvial, and aeolian deposition and by soil formation. Silt and sand layers in the lower part of the section correlate with the events of Early Holocene transgression and Middle Holocene regression of Lake Khanka. Deposition in the lowermost reaches of the Komissarovka River provides a faithful record of local Holocene landscapes controlled by level changes in Lake Khanka." @default.
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- W2901403746 date "2018-11-01" @default.
- W2901403746 modified "2023-10-14" @default.
- W2901403746 title "Holocene overbank deposition in the drainage basin of Lake Khanka" @default.
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- W2901403746 doi "https://doi.org/10.1016/j.rgg.2018.10.002" @default.
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