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    Volume 38 Issue 6
    Jun.  2013
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    Article Navigation >  Earth Science  > 2013  >  38(6): 1153-1168
    LI Wu-ping, 2013. Geochemical Characteristics of the Middle Jurassic Volcanic Rocks of Haifanggou Formation, Western Liaoning Province, North China. Earth Science, 38(6): 1153-1168. doi: 10.3799/dqkx.2013.115
    Citation: LI Wu-ping, 2013. Geochemical Characteristics of the Middle Jurassic Volcanic Rocks of Haifanggou Formation, Western Liaoning Province, North China. Earth Science, 38(6): 1153-1168. doi: 10.3799/dqkx.2013.115
    shu

    Geochemical Characteristics of the Middle Jurassic Volcanic Rocks of Haifanggou Formation, Western Liaoning Province, North China

    doi: 10.3799/dqkx.2013.115

    • School of Civil Engineering, Guangzhou University, Guangzhou 510006, China

    • Received Date: 2012-12-28
    • Publish Date: 2013-06-01
      Abstract
    • The Middle Jurassic volcanic rocks of Haifanggou formation from the western Liaoning Province is an important component of Mesozoic volcanic rocks in the Yanshan Orogenic belt. The volcanic rocks of Haifanggou formation, which are mainly composed of trachyandesite with dacite and andesite, are metaluminous calc-alkaline and high-K series. Geochemical data indicate that the Middle Jurassic volcanic rocks of Haifanggou from the western Liaoning province have the low Mg adakitic volcanic features, such as SiO2≥51.98%, Al2O3≥15.0%, MgO < 4.18% (Mg# < 0.48), Sr≥436×10-6, Yb≤2.25×10-6, Y≤23.14×10-6, Cr≤81.09×10-6, Ni≤34.66×10-6, Y/Yb≤14.25, Sr/Y≥39, and Nb/Ta≈20. The rocks are enriched in light rare earth elements (LREE), Ba, U, Sr and Pb, and are depleted in heavy rare earth elements (HREE) and high field strength elements (such as Nb, Ta, Ti), and strongly fractionated ((La/Yb)N≥10.37) with weak negative Eu anomaly or positive Eu anomaly (0.79 to 1.05 in Eu/Eu*). In addition, these adakitic volcanic rocks also have that low (143Nd/144Nd) initial ratios (0.511 603 to 0.511 733, -15.84 to -13.30 in epsilon εNd(t)), moderate (87Sr/86Sr) initial ratios (0.704 9 to 0.705 6, 8.64 to 18.11 in epsilon εSr(t)) and a higher depleted mantle model ages (1.81 to 1.99 Ga in TDM), showing enriched mantle end-member (EMI) characteristics. These features indicate that Haifanggou adakitic magma were derived from the partial melting of a thickened eclogite from the lower crust, and its origin is related to underplating of the basaltic magma. Combining with geochemistry of Mesozoic volcanic rocks in Yanshan Orogenic belt, the Early-Middle Jurassic in the Yanshan orogenic belt is a conversion period from the ancient Asian Ocean tectonic system to the paleo-Pacific tectonic system, while the generation of the Middle Jurassic adakitic volcanic rocks of Haifanggou formation (174 Ma) shows that the Yanshan orogenic belt has come into the evolution stage of the paleo-Pacific tectonic system. The research results can facilitate the understanding of the deep mechanism of Yanshan movement and lithospheric thinning process.

       

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