结果表明,镘头组下部的硅质层是同生期生物化学作用成因的,形成于潮下低能浅水环境;
The siliceous rocks of the lower Mantou formation were resulted from the biochemical action during the sedimentary period and formed in the environment of low-tide shallow sea.
结果表明,镘头组下部的硅质层是同生期生物化学作用成因的,形成于潮下低能浅水环境;
The siliceous rocks of the lower Mantou formation were resulted from the biochemical action during the sedimentary period and formed in the environment of low-tide shallow sea.
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