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- W2353179905 abstract "The shallowly buried channel zone spreads northwards in a hand shape with the alluvial fan body as the center.The fluvial deposits show evident steps:the mid time deposits are dominated by medium sized and fine sand,varying greatly in grain size,and late time deposits are mainly silt in composition.The ancient river channel can be divided into 5 parts vertically,in fining upwards tendency.According to section analysis of the drills,the ancient Weihe fluvial deposits did not shift much in cross direction,and grain sizes get finer gradually from the main stream zone to the bank sides,and change with hydrodynamic strength.The grain sizes also turn finer from the upper reaches to the lower with sorting getting much stronger.Since late Pleistocene,5 phases of ancient channels have developed in the Weihe area,corresponding with glacial and interglacial climatic changes.Among them,phases Ⅰ and Ⅱ channels had thick and coarse deposits,in good continuity in longitudinal direction and thus acting as good aquifers.Later river channels had thick but fine deposits,which served as freshwater reservoir in early time,but became a main passage for seawater to invade due to overuse of the groundwater." @default.
- W2353179905 created "2016-06-24" @default.
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- W2353179905 date "2001-01-01" @default.
- W2353179905 modified "2023-09-25" @default.
- W2353179905 title "SHALLOWLY BURIED ANCIENT CHANNELS AND QUATERNARY STRATA DIVISION IN THE LOWER REACHES OF THE WEIHE RIVER" @default.
- W2353179905 hasPublicationYear "2001" @default.
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