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    Volume 44 Issue 12
    Dec.  2019
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    Xia Feiyong, Jiao Yangquan, Rong Hui, Wu Liqun, Zhu Qiang, Wan Lulu, 2019. Geochemical Characteristics and Geological Implications of Sandstones from the Yaojia Formation in Qianjiadian Uranium Deposit, Southern Songliao Basin. Earth Science, 44(12): 4235-4251. doi: 10.3799/dqkx.2019.045
    Citation: Xia Feiyong, Jiao Yangquan, Rong Hui, Wu Liqun, Zhu Qiang, Wan Lulu, 2019. Geochemical Characteristics and Geological Implications of Sandstones from the Yaojia Formation in Qianjiadian Uranium Deposit, Southern Songliao Basin. Earth Science, 44(12): 4235-4251. doi: 10.3799/dqkx.2019.045

    Geochemical Characteristics and Geological Implications of Sandstones from the Yaojia Formation in Qianjiadian Uranium Deposit, Southern Songliao Basin

    doi: 10.3799/dqkx.2019.045
    • Received Date: 2019-03-13
    • Publish Date: 2019-12-15
    • The geochemical composition of sandstones in sedimentary basin plays an important role in the study of sedimentary provenance and tectonic settings. In this paper, detailed petrography and geochemical analyses were carried out on the sandstones of the Yaojia Formation from 4 drilling cores in the study area. All sandstone samples have the highest content of quartz (Q), followed by feldspar (F), and the lowest amount of lithic fragments (L), with an average of 42%, 37% and 21% respectively, featuring with heavy mineral assemblage of zircon-titanium magnetite-garnet, which suggests an acidic or metamorphic source. Dickinson discrimination diagrams show provenance mainly from continental block provenance. The REE distribution patterns are uniform, with LREE enrichment, flat HREE, and moderate negative Eu anomalies (average 0.63). Chemical index of alteration CIA (52.02-60.16, average 56.69) of the sandstones displays that they have experienced low grade of chemical weathering and alteration under arid paleoclimate condition. The discrimination diagrams for provenance attribute indicate a mixed source material composition of old sedimentary rocks and felsic igneous rocks. Based on major elements, trace and rare earth elements tectonic setting discrimination diagrams, suggested that source materials of the Yaojia Formation sandstones were from passive margin environment, and its provenances were from Yanshan intracontinental orogenic belts of the northern margin of Huabei Craton.

       

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