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The banded rocks have gradually changed into phyllite or slate, which show characteristics of a hydrothermal sediment basin locally depressed. 地層走向上 ，條帶狀巖石漸變過(guò)渡為千枚巖或板巖 ，顯示局部凹陷的熱水沉積盆地特點(diǎn) ；