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本文以沉积剖面旋回层为基础,提出了研究古代浅海沉积环境和古沉积的新方法。这一方法可能定量地、较精确地重现古代浅海的某些沉积环境,揭示沉积环境的演变,并对古沉积学、古构造运动以及成矿规律等的研究都具有一定的实际意义.
Based on the sedimentary section cyclotron, this paper presents a new method to study the ancient shallow marine sedimentary environment and paleosol deposition. This method may quantitatively and accurately reproduce some sedimentary environment in the shallow sea and reveal the evolution of the sedimentary environment. It is of practical significance to the study of palaeotectonics, palaeotectonic movement and metallogenic regularity.