Volume 46 Issue 9
Oct.  2021
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Lin Xu, Liu Jing, Wu Zhonghai, Liu Weiming, Li Chang'an, Li Zhiwen, Wang Shimei, Liu Haijin, Chen Jixin, 2021. Provenance of the Loess in Shandong Province (Eastern China) during the Last Ice Age: Constraints from the U-Pb Age of Detrital Zircons. Earth Science, 46(9): 3230-3244. doi: 10.3799/dqkx.2020.334
Citation: Lin Xu, Liu Jing, Wu Zhonghai, Liu Weiming, Li Chang'an, Li Zhiwen, Wang Shimei, Liu Haijin, Chen Jixin, 2021. Provenance of the Loess in Shandong Province (Eastern China) during the Last Ice Age: Constraints from the U-Pb Age of Detrital Zircons. Earth Science, 46(9): 3230-3244. doi: 10.3799/dqkx.2020.334

Provenance of the Loess in Shandong Province (Eastern China) during the Last Ice Age: Constraints from the U-Pb Age of Detrital Zircons

doi: 10.3799/dqkx.2020.334
  • Received Date: 2020-10-10
    Available Online: 2021-10-14
  • Publish Date: 2021-10-14
  • The thick loess-palaeosol sequences in the Jiaodong Peninsula and Central Shandong mountains provide high-resolution records of Late Quaternary climate change of the Shandong Province. However, it is still controversial as to where they came from. This study presents systematically the detrital zircon U-Pb age (n=420) and multi-dimensional discrimination diagram results of statistical method. It is shown that the North China Plain and Bohai shelf material served as a major dust supply for the loess in the Jiaodong Peninsula and eastern parts of the Central Shandong mountains during the Late Pleistocene. By contrast, the major dust source for the loess in the western parts of the Central Shandong mountains is mainly derived from the sediments exposed on the floodplain of the lower reaches of the Yellow River and the Loess Plateau during the Late Pleistocene. They have no provenance relationship with the sediments exposed on the sea floor in the Bohai Sea at the same time.

     

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