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    HE Zhong-hua, WANG Yu-fen, HOU Wei. Geochemistry and provenance analysis of the Middle Jurassic sandstones in the Mohe Basin,Heilongjiang[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(4): 93-100.
    Citation: HE Zhong-hua, WANG Yu-fen, HOU Wei. Geochemistry and provenance analysis of the Middle Jurassic sandstones in the Mohe Basin,Heilongjiang[J]. Sedimentary Geology and Tethyan Geology, 2008, 28(4): 93-100.
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    Geochemistry and provenance analysis of the Middle Jurassic sandstones in the Mohe Basin,Heilongjiang

    • College of Earth Sciences, Jilin University, Changchun 130061, Jilin, China

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    • Published Date: December 29, 2008
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    • The Middle Jurassic sandstones in the Mohe Basin,Heilongjiang are characterized by high contents of SiO2 and low contents of Fe2O3,FeO and MgO,LREE enrichment,HREE depletion and slightly negative Eu anomaly.The geochemical signatures of major and trace elements and REEs,in integration with the discrimination diagrams for tectonic settings have mirrored that the Middle Jurassic deposits were derived from the continental island arcs and active continental margins.The Palaeozoic complexes on the northern margin of the Ergun block may be regarded as the main provenance of the basin.
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