作者: John D. Milliman
DOI: 10.1007/978-1-4684-2754-7_23
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摘要: Inorganic precipitation of calcium carbonate, both as limestone cement and unconsolidated lutite, occurs in several types deep-sea environments. While such carbonates account for only a small part the total carbonate budget, they appear to be more important quantitatively than shallow-water precipitates. Recognizing understanding processes cementation can give added insights into sedimentation prior evolution calcareous nannoplankton Zooplankton.