Geochemistry of the Chaokeshan ophiolite: Product of intra - oceanic back - arc basin?

内蒙朝克山蛇绿岩地球化学: 洋内弧后盆地的产物?

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The 3 sedimentary melanges in the Hagong Formation ( Late Carnian - Norian ) are resulted from the back - arc riftogenesis.

哈工组 ( 卡尼晚期 ——— 诺利期 ) 中的三层沉积混杂岩是弧后裂陷作用的产物.

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The small ocean basin is formed and the ophiolite appear when back arc basin expands.

弧后盆地扩张到达小洋盆,出现蛇绿混杂岩.

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