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    Volume 37 Issue 1
    Jan.  2012
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    Article Contents
    LI Shang-lin, WANG Xun-lian, DUAN Jun-mei, LONG Wen-hua, MA Bo-yong, YANG Wen-rui, 2012. Findings and Its Geological Significance of the Upper Devonian Ophiolite in Hujierte Area, Damao County, Inner Mongolia, China. Earth Science, 37(1): 18-24. doi: 10.3799/dqkx.2012.002
    Citation: LI Shang-lin, WANG Xun-lian, DUAN Jun-mei, LONG Wen-hua, MA Bo-yong, YANG Wen-rui, 2012. Findings and Its Geological Significance of the Upper Devonian Ophiolite in Hujierte Area, Damao County, Inner Mongolia, China. Earth Science, 37(1): 18-24. doi: 10.3799/dqkx.2012.002

    Findings and Its Geological Significance of the Upper Devonian Ophiolite in Hujierte Area, Damao County, Inner Mongolia, China

    doi: 10.3799/dqkx.2012.002
    • Received Date: 2010-05-26
    • Publish Date: 2012-01-15
    • Assemblages of the Upper Devonian ultrabasic rock, cumlative complex, diabase-dike swarm as well as basic pillow lava nipping radiolarian Si-sargillaceous rocks are discovered in Hujierte area, Inner Mongolia, China. They are typical ophiolite, which geochemical compositions accord with the characteristics of MORB. The age of 371.0±5.3 Ma using zircon U-Pb geologic dating method shows that there is the Upper Paleozoic era oceanic crust in this area, being a part of the Paleo-Asiatic Ocean, it is possibly a branch of ocean basin in archipelago paleogeographic pattern between the Siberian plate and the Sino-Korean plate, not inner the Sino-Korean plate, a northern part of the Sino-Korean plate should be on the south of Hujierte at the least.

       

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