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Karbon je geologický útvar prvohor (paleozoikum) a jde tedy také o součást eónu fanerozoika. Počátek karbonského útvaru je kladen 354 milionů let (Ma) zpět do minulosti a jeho spodní hranice je vymezena nástupem druhu Siphonodella sulcata, což je drobný konodont (Conodonta).
Paleoklimatické poměry, Biosféra & Regionální přehled
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spodní slepence karbonu jsou namur svrchní prachovce sedimenty pískovce slojí vestfál mocnost tzv km visé mořské stefan sedimentace stáří mocnosti
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Karbon | related to Asie | Při | 0.60 | section |
| Karbon | related to Asie | Asie | 0.60 | section |
| Karbon | related to Asie | Podstatné | 0.60 | section |
| Karbon | related to Asie | Ve | 0.60 | section |
| Karbon | related to Asie | Kavkaz | 0.60 | section |
| Karbon | related to Asie | Pamír | 0.60 | section |
| Karbon | related to Asie | Himálaj | 0.60 | section |
| Karbon | related to Asie | Kontinentální | 0.60 | section |
| Karbon | related to Britské ostrovy | Spodní | 0.60 | section |
| Karbon | related to Britské ostrovy | Anglii | 0.60 | section |
| Karbon | related to Britské ostrovy | Cornwall | 0.60 | section |
| Karbon | related to Britské ostrovy | Devon | 0.60 | section |
These clusters group vocabulary that occurs around closely connected concepts in the source material.
Bridges can reveal useful research angles that are easy to miss in a flat list of related terms.