With stromatolite but no desiccation crack, the depositional environment of Middle-Late Cambrian in the area was intertidal zone to subtidal zone with the shallow-water features.
根据其中的叠层石和无明显泥裂构造，推测为
间带-局
带沉积环境。
With stromatolite but no desiccation crack, the depositional environment of Middle-Late Cambrian in the area was intertidal zone to subtidal zone with the shallow-water features.
根据其中的叠层石和无明显泥裂构造，推测为间带-局带沉积环境。
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