Turbiditischer Kalkstein aus der Kreidezeit mit Paleodictyon minutum
Kalkstein, turbiditisch, mit Bouma-Zyklus, Paleodictyon minutum KINDELAAM und Spuren auf Sohlfläche. Ober-Campanium, mucronata-Zone, minor-Subzone, untere Vorhelm-Formation. Erweiterung des Neuen Steinbruchs der Firma Bosenberg Zement, Ahlen-Vorhelm 2002.
Die Beschreibung einer Bouma-Sequenz findet ihr bei Wikipedia unter https://de.wikipedia.org/wiki/Bouma-Sequenz.
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| Sections | Natur: Natur-Makros Natur: Steine & Mineralien Natur: Fossilien & Präparate |
| Folders | Minerale•Fossilien |
| Views | 1,926 |
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