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- W2364862548 abstract "Mountain land erosion and plain accumulation are two different representations of physiographic time.Based on the correlation among,coarsely granular material at the lower part of plain,fine granular material at the upper part of the plain and the surface weathered crust or paleosoil,this paper renamed the physiographic time of North China,which are as follows: the late Cretaceous Period physiographic time is presented as Beitai Period Erosion-Lugou bridgeand Wuji Period Accumulation;the early Tertiary Period physiographic time is presented as Dianziliang, Period Erosion-Kongdian and Shahe River Period Accumulation;the late Tertiary Period physiographic time is presented as Tang County Period Erosion-Guantao and Minghua Town Period Accumulation;the early Pleistocene Epoch physiographic time is presented as Fenhe River Period Erosion-Gu'an Period Accumulation;the middle Pleistocene Epoch physiographic time is presented as Huangshui Period Erosion-Yangliuqing Period Accumulation;the late Pleistocene Epoch physiographic time is presented as Qingshui Period Erosion-Ouzhuang Period Accumulation;the early and the middle Holocene physiographic time is presented as Banqiao Period Erosion-Yangjiasi and Gaowan Period Accumulation;the late Holocene physiographic time is presented as Duanqu Period Erosion-Qikou Period Accumulation." @default.
- W2364862548 created "2016-06-24" @default.
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- W2364862548 date "2005-01-01" @default.
- W2364862548 modified "2023-09-28" @default.
- W2364862548 title "A New Viewpoint on Renaming the Physiographic Time of North China" @default.
- W2364862548 hasPublicationYear "2005" @default.
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