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    Volume 40 Issue 3
    Mar.  2015
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    Article Contents
    Zong Ruiwen, Gong Yiming, Han Fei, 2015. Discovery of Silurian Fossils and Its Geological Significance in Eastern Emin, Xinjiang of NW China. Earth Science, 40(3): 563-572. doi: 10.3799/dqkx.2015.044
    Citation: Zong Ruiwen, Gong Yiming, Han Fei, 2015. Discovery of Silurian Fossils and Its Geological Significance in Eastern Emin, Xinjiang of NW China. Earth Science, 40(3): 563-572. doi: 10.3799/dqkx.2015.044

    Discovery of Silurian Fossils and Its Geological Significance in Eastern Emin, Xinjiang of NW China

    doi: 10.3799/dqkx.2015.044
    • Received Date: 2014-04-04
    • Publish Date: 2015-03-15
    • Abundant Wenlock animal fossils are found in the succession of the volcanoclastic rocks intercalated with limestones which were considered as the Late Devonian Ta'erbahatai Formation, including corals Halysites hoboksarensis, H. sp., Mesofavosites sp., brachiopods Atrypa sp., Eospirifer radiates, trilobites Encrinuroides sp., Encrinurus sp.1, E. sp.2, Cheirurus sp., Sthenarocalymene sp., Machaeridia Lepidocoleus sp., stromatoporoids and so on. Based on lithological association and stratal correlation, the succession is re-assigned to the Wenlock Shaerbuer Formation, where abundant facies indicators were discovered. Main facies indicators include reefoid corals and stromatoporoids, graded bedding, convolute bedding, flame structure and storm deposits. It is concluded that the Wenlock Shaerbuer Formation was formed in the open platform environment with volcanic activities in tropical and subtropical zones.

       

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