南华系建系问题探讨PROBLEMS IN DEFINING THE NANHUAN PERIOD
张启锐,储雪蕾
摘要(Abstract)：
南华系的研究与关于成冰系的研究配合不多,把南华系简单地理解为原震旦系下统,侧重于原震旦系下统底界年龄的测定,把国外给定的关于"成冰系"的起始年龄值(即850Ma)看得过重,忽略了它的不确定性。对于作为南华系主体的新元古代冰期地层的研究比较薄弱,与国际冰川沉积学研究水平差距大。为此,有必要根据界线层型剖面的要求开展建系工作,重点深入研究新元古代冰川沉积地层的基本特征,包括层序地层学、同位素地层学、磁性地层学、岩石地层学、化学地层学、生物地层学和年代地层学等,明确其内涵,寻找全球对比的界线标志。建议以贵州黎平肇兴剖面为代表开展候选层型剖面和层型点所需内容研究。
关键词(KeyWords)： 南华系;成冰系;冰期地层;界线层型剖面;肇兴剖面;黎平;贵州
基金项目(Foundation): 国家自然科学基金重点项目(No40532012);; 中国科学院知识创新工程项目(NoKZCX3-SW-141)资助
作者(Author): 张启锐,储雪蕾
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