必死 发表于 2025-3-25 03:23:11

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飞镖 发表于 2025-3-25 10:59:56

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angina-pectoris 发表于 2025-3-25 13:25:12

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拥挤前 发表于 2025-3-25 16:10:39

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onlooker 发表于 2025-3-25 23:28:15

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geometrician 发表于 2025-3-26 02:50:42

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有权威 发表于 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.

Synchronism 发表于 2025-3-26 09:41:57

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Living-Will 发表于 2025-3-26 15:45:07

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dearth 发表于 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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查看完整版本: Titlebook: Coated Grains; Tadeusz M. Peryt Conference proceedings 1983 Springer-Verlag Berlin Heidelberg 1983 Dolomite.Gestein.Karbonatgestein.Konkre