2018
DOI: 10.1007/978-981-10-7638-1_1
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Late Quaternary Landform Development of the Kanto Plain

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Cited by 1 publication
(2 citation statements)
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“…Clayey silt is present from a depth of 16 to 20 m; it could be described as transitional sediment after confirming its physicochemical data from Figure 3 and with reference [30]. Marine sediment is distributed from 20 to 27 m. sediment thickness was confirmed from the EC value, S content, the presence of marine shell fragments, and correlation with other references [30,32,43,44]. Marine sediment is separated from nonmarine sediment by 3 m of transitional sediment ( Figure 2).…”
Section: Lithologic Reconstructionsupporting
confidence: 72%
See 1 more Smart Citation
“…Clayey silt is present from a depth of 16 to 20 m; it could be described as transitional sediment after confirming its physicochemical data from Figure 3 and with reference [30]. Marine sediment is distributed from 20 to 27 m. sediment thickness was confirmed from the EC value, S content, the presence of marine shell fragments, and correlation with other references [30,32,43,44]. Marine sediment is separated from nonmarine sediment by 3 m of transitional sediment ( Figure 2).…”
Section: Lithologic Reconstructionsupporting
confidence: 72%
“…A lithological column was performed after correlating with the relevant references of nearby areas and collecting physicochemical data of the sediment samples, e.g., visual observations of the color, particle size distribution, electrical conductivity, and S content ( Figure 2). The lithostratigraphic reconstruction and landform evolution in the Kanto Plain have been studied by different parties [29,32,[42][43][44], and research there is ongoing. For this research, the sediments of different depositional environments were identified and described, along with the chemical characteristics.…”
Section: Lithologic Reconstructionmentioning
confidence: 99%