BiCoNi Formation (original) (raw)
The BiCoNi Formation is a hydrothermal lode formation, in which bismuth, cobalt, nickel and uranium ores have coalesced. It occurs mainly in the Ore Mountains and is the youngest formation in the hydrothermal sequence (polymetalliferous (kb) formation, iron-barite (eba) formation, precious brownspar (eb) formation, fluorite-barite (fba) formation, BiCoNi formation). Due to its combination with uranium, it is occasionally also called the bismuth-cobalt-nickel-uranium formation.
| Property | Value |
|---|---|
| dbo:abstract | The BiCoNi Formation is a hydrothermal lode formation, in which bismuth, cobalt, nickel and uranium ores have coalesced. It occurs mainly in the Ore Mountains and is the youngest formation in the hydrothermal sequence (polymetalliferous (kb) formation, iron-barite (eba) formation, precious brownspar (eb) formation, fluorite-barite (fba) formation, BiCoNi formation). Due to its combination with uranium, it is occasionally also called the bismuth-cobalt-nickel-uranium formation. (en) Die BiCoNi-Formation ist eine hydrothermale Gangformation, in der Wismut-, Kobalt-, Nickel- und Uranerze miteinander verwachsen sind. Sie tritt hauptsächlich im Erzgebirge auf und ist die jüngste Formation in der hydrothermalen Abfolge (kb-Formation, eba-Formation, eb-Formation, fba-Formation, BiCoNi-Formation). Wegen der Verknüpfung mit Uran wird sie gelegentlich auch als Wismut-Kobalt-Nickel-Uran-Formation bezeichnet. (de) |
| dbo:wikiPageExternalLink | http://www.geo.tu-freiberg.de/Hauptseminar/2009/Marco_Muench.pdf%7Cformat=PDF, http://www.igf-bbg.de/adobe/1210.pdf%7Cformat=PDF, https://publikationen.sachsen.de/bdb/artikel/12174/documents/11794%7Caccess-date= https://publikationen.sachsen.de/bdb/artikel/12540%7Caccess-date= |
| dbo:wikiPageID | 53652697 (xsd:integer) |
| dbo:wikiPageLength | 3702 (xsd:nonNegativeInteger) |
| dbo:wikiPageRevisionID | 953517006 (xsd:integer) |
| dbo:wikiPageWikiLink | dbc:Geology_of_Germany dbr:Ore dbr:Cobalt dbr:Late_Middle_Ages dbr:Lode dbr:Nickel dbr:Intrusion_(geology) dbr:Hydrothermal_circulation dbr:Arsenide dbr:Bismuth dbr:Wismut_(company) dbr:Pitchblende dbr:Native_element_minerals dbr:Ore_Mountains dbr:Slate dbr:Uranium dbr:Variscan_orogeny dbr:Paragenesis |
| dbp:wikiPageUsesTemplate | dbt:Citation dbt:Cite_web |
| dct:subject | dbc:Geology_of_Germany |
| rdfs:comment | The BiCoNi Formation is a hydrothermal lode formation, in which bismuth, cobalt, nickel and uranium ores have coalesced. It occurs mainly in the Ore Mountains and is the youngest formation in the hydrothermal sequence (polymetalliferous (kb) formation, iron-barite (eba) formation, precious brownspar (eb) formation, fluorite-barite (fba) formation, BiCoNi formation). Due to its combination with uranium, it is occasionally also called the bismuth-cobalt-nickel-uranium formation. (en) Die BiCoNi-Formation ist eine hydrothermale Gangformation, in der Wismut-, Kobalt-, Nickel- und Uranerze miteinander verwachsen sind. Sie tritt hauptsächlich im Erzgebirge auf und ist die jüngste Formation in der hydrothermalen Abfolge (kb-Formation, eba-Formation, eb-Formation, fba-Formation, BiCoNi-Formation). Wegen der Verknüpfung mit Uran wird sie gelegentlich auch als Wismut-Kobalt-Nickel-Uran-Formation bezeichnet. (de) |
| rdfs:label | BiCoNi-Formation (de) BiCoNi Formation (en) |
| owl:sameAs | wikidata:BiCoNi Formation dbpedia-de:BiCoNi Formation https://global.dbpedia.org/id/aDX9 |
| prov:wasDerivedFrom | wikipedia-en:BiCoNi_Formation?oldid=953517006&ns=0 |
| foaf:isPrimaryTopicOf | wikipedia-en:BiCoNi_Formation |
| is dbo:wikiPageRedirects of | dbr:BiCoNi |
| is dbo:wikiPageWikiLink of | dbr:Black_Forest dbr:BiCoNi |
| is foaf:primaryTopic of | wikipedia-en:BiCoNi_Formation |