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本文根据实际资料,简要概括了中国大陆架海绿石的分布规律和形成环境。海绿石的富集区与氧化环境,粗粒沉积和残留沉积区相一致。该研究为恢复古沉积环境提供了依据。
Based on the actual data, this article gives a brief summary of the distribution and formation of glauconite in the continental shelf of China. The glauconitic enrichment zone is consistent with the oxidizing environment, coarse-grained sediments and residual sedimentary zones. The study provided the basis for restoration of paleodial depositional environment.