These Devonian volcanics were resulted from the subduction of oceanic lithosphere basin (between Heiying Mountains and Hula Mountains) in south rim of South Tianshan to the north in early Devonian.
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释义
该套火山岩由于南天山南缘洋盆(黑英山-虎拉山间的洋盆)在早泥盆世中期向北俯冲而成。
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