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文章对晚元古代冰碛岩和似冰碛岩层的地层位置作了分析。分析结果证明,它们处于两个层位:850—820百万年和680—650百万年。根据古地理特点,确定了原始的和再沉积的典型冰碛岩和冰水沉积。对晚里菲期和早温特期的气候条件作了分析。根据气候的分带性,对仅基于古地磁资料的大陆位置模型的可靠性提出质疑,并列举出里菲期末和温特期岩石圈板块的另一种奇异的图景。
The paper analyzes the stratigraphic position of late moraine and moraine rock strata. The analysis shows that they are in two horizons: 850-820 million years and 680-650 million years. Based on paleogeographical features, the primitive and redeposited typical moraine and glacial water deposits were identified. The climatic conditions of late Philippine and early Winter are analyzed. According to the zonality of the climate, the reliability of the continental location model based solely on paleomagnetic data is questioned, and another singular picture of the lithospheric plate at the end of the Riffy and Winter Periods is listed.