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    中国百强科技报刊

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    中国高校百佳科技期刊

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    Volume 40 Issue 3
    Mar.  2015
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    Article Contents
    Yang Wei, Wang Guocan, Zong Ruiwen, Xiao Long, Li Li, Yang Gang, 2015. Determination of Silurian-Devonian Arc-Basin Pattern in Western Junggar and Its Regional Tectonic Significance. Earth Science, 40(3): 448-460,503. doi: 10.3799/dqkx.2015.037
    Citation: Yang Wei, Wang Guocan, Zong Ruiwen, Xiao Long, Li Li, Yang Gang, 2015. Determination of Silurian-Devonian Arc-Basin Pattern in Western Junggar and Its Regional Tectonic Significance. Earth Science, 40(3): 448-460,503. doi: 10.3799/dqkx.2015.037

    Determination of Silurian-Devonian Arc-Basin Pattern in Western Junggar and Its Regional Tectonic Significance

    doi: 10.3799/dqkx.2015.037
    • Received Date: 2014-08-02
    • Publish Date: 2015-03-15
    • Paleozoic substance formations are widespread in Karamay-Emin area of western Junggar in Xinjiang, recording evolution information of Paleo-Asian Ocean. During Paleozoic, and especially the Late Paleozoic, this region has experienced a complex ocean-land transition process. Thus, a series of ophiolitic mélanges with nearly east-west and northeastern trends, and subduction-accretionary complexes of the ancient continental margin have been developed, resulting in the complicated rock formation system in the study area. To better probe into the ancient geographical attributes and structural framework between Silurian and Devonian in western Junggar, we define the tectonic paleogeographic properties of Silurian and Devonian in Karamay-Emin area and discuss arc-basin tectonic framework from Silurian to Devonian in western Junggar based on geological survey and relevant data in this study. The authors suggest that Paleo-Asian Ocean in the Karamay-Emin area began intense subducting in Silurian and widely subduction-collage stage with archipelago arc-basin system in Devonian. Paleo-Asian Ocean along the Karamay-Emin area started its residual oceanic basin evolutionary stage after Devonian.

       

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