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2023 Vol. 50, No. 6
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TAO Rui, HAI Lianfu, WANG Lei, SONG Yang, LI Haifeng, LIN Li, MEI Chao, BAI Jinhe. 2023. Geochemical characteristics of clastic rocks from the Jurassic Zhiluo Formation in Lingwu, Ningxia and analysis of tectonic background of the source area[J]. Geology in China, 50(6): 1817-1836. doi: 10.12029/gc20200303001
Citation: TAO Rui, HAI Lianfu, WANG Lei, SONG Yang, LI Haifeng, LIN Li, MEI Chao, BAI Jinhe. 2023. Geochemical characteristics of clastic rocks from the Jurassic Zhiluo Formation in Lingwu, Ningxia and analysis of tectonic background of the source area[J]. Geology in China, 50(6): 1817-1836. doi: 10.12029/gc20200303001
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Geochemical characteristics of clastic rocks from the Jurassic Zhiluo Formation in Lingwu, Ningxia and analysis of tectonic background of the source area

  • 1.

    Ningxia Institute of Mineral Geological Survey (Autonomous Region Institute of Mineral Geology), Yinchuan 750021, Ningxia, China

  • 2.

    College of Resources China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

  • 3.

    Chengdu University of Technology, Chengdu 610059, Sichuan, China

    • Fund Project: Supported by the projects of Ningxia Natural Science Foundation (No.2021AAC03446) and the Ningxia Excellent Talent Support Program (No.JTGC2019023)
More Information
  • Author Bio: TAO Rui, male, born in 1990, Ph.D., mainly engaged in geological mineral survey and petrology research; E-mail: 18384127744@163.com
  • Corresponding author: HAI Lianfu, male, born in 1989, Ph.D. candidate, mainly engaged in geological and mineral survey; E-mail: 791128985@qq.com 
Received Date:  03 March 2020
Revised Date:  03 June 2020
Publish Date:  25 December 2023
    Abstract

  • This paper is the result of geological survey engineering.

     Objective

    The Zhiluo Formation represents a transitional phase in the lake's advancement and retreat within the broader context of Jurassic geological evolution. Its tectonic background holds paramount importance in exploring the inception timeline of fault-fold belt development along the western margin of the Ordos Basin. This study focuses on the Zhiluo Formation, specifically clastic rocks, from the Jurassic period in the Lingwu area, Ningxia.

     Methods

    We conducted analyses using X-ray and ICP-MS techniques to uncover the geochemical characteristics of clastic rocks and the structural context of the source region.

     Results

    Our results reveal that major element correlation coefficients are generally low, while trace elements and REE exhibit high values. Notably, correlation coefficients between Al2O3 and trace elements such as Co, Ni, Cr, V, Sc, Li, Cs, Be, Ga, Tl, Cu, Pb, Zn, and Sn exceed 0.9, and the correlation coefficients between TiO2 and Nb are at 0.98. This suggests that the primary source of sediment is terrigenous clastic material. Enrichment concentration-type elements (K>1, CV>1) include Zr, U, and CaO, while enrichment dispersion-type elements (K>1, CV < 1) consist of Al2O3, Fe2O3, MgO, Sr, Ba, U, Co, V, Sc, Li, and Pb. Poorly dispersive elements (K < 1, CV < 1) encompass SiO2, TiO2, MnO, Na2O, K2O, P2O5, Rb, Th, Nb, Ta, Ni, Cr, Cs, Be, Ga, Tl, Cu, Zn, As, Sn, and REE. No elements fall under the poor concentration type (K < 1, CV>1).

     Conclusions

    The average values for key oxide combinations of main elements are TiO2 (0.54), TFe2O3+MgO (4.58), Al2O3/SiO2 (0.58), and Al2O3/SiO2 (0.18), indicating similarity to an active continental margin. A trace element spider diagram demonstrates the rocks of the Zhiluo Formation's richness in Rb, K, and U, which are large ion lithophile elements, and a significant deficit in Nb, Sr, P, and Ti. The chondrite-standardized REE distribution curve depicts a gentle right-leaning pattern, signifying LREE enrichment and HREE relative depletion. In terms of geochemical indices, the CIA (70.76-81.88) for mudstone exceeds the ICV (1.02-1.6) for sandstone, while mudstone ICV (0.7-1.14) remains mostly less than or equal to 1. This suggests that the Zhiluo Formation in the Lingwu area exhibits little to no recycling and is characteristic of primary sedimentation in the context of tectonic activity with a moderate degree of differentiation. Correlation diagrams indicates that tectonic background of the source region is primarily associated with an active continental margin. Additionally, it exhibits some links to continental island arc systems, suggesting an active continental margin or an active continental margin subduction zone, potentially resembling an Andean-type active continental margin.
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