• The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest tran

    更新世更新世早期弱,仅有海过渡相沉积

    youdao

  • The transgressions of Middle Pleistocene and the early Late Pleistocene were weak and represented by deposits of the transitional nature from marine to continental facies only. The strongest tran

    更新世更新世早期弱,仅有海过渡相沉积

    youdao

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