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    Volume 33 Issue 6
    Jun.  2008
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    JIN Song, ZHANG Li, ZHONG Zeng-qiu, ZHOU Han-wen, XIANG Hua, CENG Wen, LIU Rui, LU: Xin-qian, LI Chun-zhong, 2008. Geochemical Characteristics and Geological Implications for the Neoproterozoic Meta-Sedimentary Rocks of the Cathaysia Block in Zhejiang and Fujian Provinces. Earth Science, 33(6): 764-774.
    Citation: JIN Song, ZHANG Li, ZHONG Zeng-qiu, ZHOU Han-wen, XIANG Hua, CENG Wen, LIU Rui, LU: Xin-qian, LI Chun-zhong, 2008. Geochemical Characteristics and Geological Implications for the Neoproterozoic Meta-Sedimentary Rocks of the Cathaysia Block in Zhejiang and Fujian Provinces. Earth Science, 33(6): 764-774.

    Geochemical Characteristics and Geological Implications for the Neoproterozoic Meta-Sedimentary Rocks of the Cathaysia Block in Zhejiang and Fujian Provinces

    • Received Date: 2008-02-28
    • Publish Date: 2008-11-25
    • The upper basement of the Cathaysia block in Zhejiang and Fujian provinces consists mainly of the Neoproterozoic Longquan Group, Mamiansban Group, and Wanquan Group. These three groups exhibit similarity in rock assemblage as well as major and trace elements geochemistry. They are the main components of the uniform upper basement of the Cathaysia block, consisting mainly of schists, leptynites, quaterizes and marbles. Schists and the leptynites have variable composi-tions, with SiO2 contents ranging from 52.89% to 75.03%, TiO2 from 0.48% to 1.05%, Al2O3 from 9.19% to 20.3%, ∑REE between 149×10-6 and 323×10-6, δEu values between 0.34 and 0.80, and (La/Yb)N values between 7.96 and 15.6. The REE patterns display medium to high negative Eu anomaly with obvious fractionation between LREE and HREE. The quartzites have different compositions, with SiO2 contents varying from 95.49% to 97.44%, and relatively low ∑REE contents (8.89× 10-6 to 15.1 × 10-6). It is proposed that protoliths of the schists and the leptynites are wackes and clay rocks, whereas protoliths of the quartzites are ferruginous silica rocks, mainly quartz-feldspathic; and some protoliths show geochemical characteristics of ancient allochthonous sediments. The meta-sedimentary rocks of the Longquan Group, Mamianshan Group, and Wanquan Group were probably formed in an environment of arc-active continental margin. The lower maturity implies that they are near field sediments, similar to the metamorphic rock system of the lower basement in this area (Paleoproterozoic Tianjingping Formation, Badu Group, Chencai Group and Mayuan Group), analogous to the upper crustal rocks.

       

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