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《Journal of Stratigraphy》 2007-02
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SUBDIVISION AND CORRELATION OF THE LATE PLEISTOCENE—HOLOCENE STRATA IN THE BAOTOU AREA AND ITS PALEOENVIRONMENT VARIATION

DENG Jin-xian, LIU Zheng-hong, XU Zhong-yuan, YANG Zhen-sheng, WEN Quan-bo, LI Feng-jiang and SONG Hai-fengCollege of Earth Science, Jilin University, Changchun, 130026  
Chronostratigraphic, biostratigraphic, lithostratigraphic, and magnetostratigraphic investigation of the Neogene sediments of the Baotou Plain suggests that the late Pleistocene—Holocene strata may be correlated with the Dishaogouwan profile at the Salawusu River, a Pleistocene—Holocene type section in North China. The strata can be further subdivided into the Salawusu Formation, Chengchuan Formation, Dagouwan Formation, and Dishaogouwan Formation. The study not only revises the Neogene stratigraphy in the Baotou Plain, which facilitates regional stratigraphic correlation, but also provides stratigraphic data for the study of Neogene paleoclimatic and paleogeographic changes in the Baotou area and the Hubao Basin.
【Fund】: 中国地质调查局1/25万《包头幅》区域地质调查(No.200113000021)。
【CateGory Index】: P534.63
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