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    Wu Zijie, Zhang Guoren, Qiu Longwei, Wang Haipeng, Zhong Mishan, Gao Fuliang, Pan Yuqi, Luo Niangang. 2024. Geochemical characteristics of sandstone and sedimentary background of Neoproterozoic Qiaotou Formation in Liaoning[J]. Geology in China, 51(5): 1714−1726. DOI: 10.12029/gc20200919002
    Citation: Wu Zijie, Zhang Guoren, Qiu Longwei, Wang Haipeng, Zhong Mishan, Gao Fuliang, Pan Yuqi, Luo Niangang. 2024. Geochemical characteristics of sandstone and sedimentary background of Neoproterozoic Qiaotou Formation in Liaoning[J]. Geology in China, 51(5): 1714−1726. DOI: 10.12029/gc20200919002
    shu

    Geochemical characteristics of sandstone and sedimentary background of Neoproterozoic Qiaotou Formation in Liaoning

    • 1.

      Liaoning Institute of Geological Exploration Co., Ltd, Dalian 116100, Liaoning, China

    • 2.

      School of Geosciences, China University of Petroleum (East China), Qingdao 266580, Shandong, China

    • 3.

      Fossil Protection Technology Innovation Center of Liaoning Geological Exploration and Mineral Group, Dalian 116100, Liaoning, China

    • 4.

      College of Earth Sciences, Changchun 130061, Jilin, China

    • 5.

      Shenyang University of Technology, Shenyang 110870, Liaoning, China

    Funds: Supported by the projects of Liaoning Provincial Geological Exploration and Mining Group (No.2017−03, No.2016−01)，China Geological Survey (No.1212011120734) and Liaoning Bureau of Geology and Mineral Resources (No.1994−15).
    More Information
    • Author Bio:

      WU Zijie, male, born in 1987, professor level senior engineer, mainly engaged in sedimentology and petrology; E-mail: midnight29@163.com

    • Corresponding author:

      QIU Longwei, male, born in 1967, professor, mainly engaged in sedimentology and reservoir geology; E-mail: qiulwsd@163.com

      GAO Fuliang, male, born in 1987, senior engineer, mainly engaged in petrology; E-mail: kevinangus@sina.com.

    • Received Date: September 18, 2020
    • Revised Date: December 11, 2020
      Graphical Abstract
      • Abstract

    • This paper is the result of geological survey engineering.

      Objective 

      The sedimentary period of the Qiaotou Formation in Liaoning is still not accurately determined, which leads to controversial discussions about its depositional background, especially the palaeoclimate. It is of great significance to discuss its depositional background by using petrogeochemical characteristics and other methods.

      Methods 

      We reconstructed the palaeo−weathering climate conditions, palaeo−salinity and palaeo−oxidation−reduction conditions by analysing the elemental ratios of CaO/(CaO+Fe), Sr/Ba, and V/(Ni+V), as well as the parameters of CIA, ICV, and Ceanom from the petrogeochemical data of the sandstones of the Qiaotou Formation.

      Results 

      Most of the CIA values of the sandstone samples from the Qiaotou Formation are located in the warm and humid region, while most of the ICV values are located in the cold and dry region. Most of the CaO/(CaO+Fe) and Sr/Ba values of the samples fall into the medium saline region, and a small amount is in the slightly saline region. V/(Ni+V) and Ceanom values of sandstone samples are in the reduced region, and a small amount is in the oxidised region.

      Conclusions 

      The Qiaotou Formation was not deposited in the Nanhua Period, and its depositional period was generally in an anoxic reducing environment with medium saline water and a warm and humid climate.

      Highlights
      (1) We discuss the depositional background of the Qiaotou Formation by using rock geochemical characteristics and combining evidence from various aspects such as sedimentary tectonics, rocks and minerals. (2) Through the results of the discussion on the depositional background of the Qiaotou Formation, it is hypothesised that the Qiaotou Formation was not deposited in the Nanhua Period.
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      • References (92)
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