The Kelamaili oceanic shell should subduct toward its both sides in Early Carboniferous because there are two island arc stratigraphic sequences in/on both sides of the oceanic basin sequence.

 
  • 根據克拉麥里造山帶兩側均存在島弧盆地層序,推論克拉麥里洋盆曾在早石炭世向兩側發(fā)生俯沖。
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