Volume 46 Issue 8
Aug.  2021
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Li Chen, Chen Shiyue, Lou Da, Fu Lixin, Yan Jihua, 2021. Geochemical Characteristics and Signatures of Mesozoic Sandstones from Huanghua Depression. Earth Science, 46(8): 2903-2918. doi: 10.3799/dqkx.2020.325
Citation: Li Chen, Chen Shiyue, Lou Da, Fu Lixin, Yan Jihua, 2021. Geochemical Characteristics and Signatures of Mesozoic Sandstones from Huanghua Depression. Earth Science, 46(8): 2903-2918. doi: 10.3799/dqkx.2020.325

Geochemical Characteristics and Signatures of Mesozoic Sandstones from Huanghua Depression

doi: 10.3799/dqkx.2020.325
  • Received Date: 2020-07-01
    Available Online: 2021-09-14
  • Publish Date: 2021-08-15
  • In Mesozoic, the Huanghua Depression was located in the center of the convergence and destruction of the North China Craton and was the sink place of all source areas. It recorded the evolution of the tectonic and provenance of the Mesozoic basins in North China. The main and trace elements of Mesozoic sandstones from the study area were examined. It is found that the average contents of SiO2, Al2O3, Na2O, K2O, and Fe2O3T are 66.98%, 13.65%, 2.74%, 3.03%, and 3.26%, respectively. The sandstones are litharenites, arkoses, and greywackes. The average CIA and ICV values are 56.12 and 0.94, and the sandstones experienced some chemical weathering and recycling. The parent rocks of the sandstones are feldspathic igneous rocks and recycling sedimentary rocks, mixed with a small amount of basic igneous rocks. From the Triassic to the Cretaceous, the source of Mesozoic sandstones gradually evolved from continental arc in the northern margin of North China to the paleo-uplift and the interplate magmatic area of the Yanshan orogenic belt and the Huanghua Depression.

     

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