Titlebook: Coated Grains; Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre

只看該作者 · 發(fā)表于 2025-3-26 07:35:17

https://doi.org/10.1007/978-3-319-77134-2 These grains are classified according to their structure and environmental parameters (Peryt, this vol.). Peloids are micritic grains without recognizable structures and are represented by individual grains and aggregates. Ooids, oncoids, rhodoids, and vadoids are coated grains with distinct structural features.

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只看該作者 · 發(fā)表于 2025-3-26 18:13:02

Looking to Brain Research for Insights,hamas (Illing 1954, Newell et al. 1960). This structure is normal for recent ooids from marine environments (for exceptions see Land et al. 1979). The μm-sized aragonite crystals are rod- or baton-shaped (Fabricius and Klingele 1970, Loreau 1970).

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