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1999: THE RELATIONSHIP BETWEEN THE RED SOIL AND LOESS PALEOSOL SEQUENCE IN JINGLE, SHANXI PROVINCE, AND YULIN, SHAANXI PROVINCE. Geological Bulletin of China, 18(1).
Citation: 1999: THE RELATIONSHIP BETWEEN THE RED SOIL AND LOESS PALEOSOL SEQUENCE IN JINGLE, SHANXI PROVINCE, AND YULIN, SHAANXI PROVINCE. Geological Bulletin of China, 18(1).

THE RELATIONSHIP BETWEEN THE RED SOIL AND LOESS PALEOSOL SEQUENCE IN JINGLE, SHANXI PROVINCE, AND YULIN, SHAANXI PROVINCE

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  • Available Online: August 16, 2023
  • Published Date: February 14, 1999
  • Magnetostratigraphic measurements and correlation of layers A, B and C of red soil show: (1) the Jingle red soil at Jingle and Hefeng is just layer A of red soil, in which the Gauss normal polarity zone is recorded, with an age of 2.50~3.00 Ma, corresponding to late Pliocene. Red soil in the Yulin section records the Gauss normal and Gilbert reversal polarity zones, whose age is 2.50~5.00 Ma, corresponding to Pliocene. (2) Layer B of red soil in the Jingle section, which corresponds to layer W S 1 , layer W S 2 , layer W S 3 or layer S 15 S 32 of the loess paleosol sequence, records the Olduvai and Reunion normal polarity subzones, and the age is 1.20~2.30 Ma, corresponding to early Early Pleistocene. (3) Layer C of red soil along the Yulin River bank corresponds mainly to the Lishi loess, about the S 1 S 15 interval, and partially to the Wucheng loess.

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