The Kibaran orogeny is a term that has been used for a series of orogenic events, in what is now Africa, that began in the Mesoproterozoic, around 1400 Ma and continued until around 1000 Ma when the supercontinent Rodinia was assembled.The term "Kibaran" has often been used for any orogenic rocks formed during this very extended period.Recently, it has been proposed that the term should be used in a much narrower sense for an event around 1375 Ma and a region in the southeast of the Democratic Republic of the Congo (DRC).
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| - Kibaran orogeny (en)
- Кібарська складчастість (uk)
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| - Кібарська складчастість — корелює з дальсландською складчастістю. Кібарська складчастість проявлена в Африці. Гірські породи Кібарської складчастості мають абсолютний вік близько 1 млрд років. Шуберт і Фор-Мюре (1967) зіставляють кібарську складчастість та Ірумідську складчастість з дальсландською і гренвільською, датуючи їх абсолютний вік відповідно 1000 і 900 млн років. (uk)
- The Kibaran orogeny is a term that has been used for a series of orogenic events, in what is now Africa, that began in the Mesoproterozoic, around 1400 Ma and continued until around 1000 Ma when the supercontinent Rodinia was assembled.The term "Kibaran" has often been used for any orogenic rocks formed during this very extended period.Recently, it has been proposed that the term should be used in a much narrower sense for an event around 1375 Ma and a region in the southeast of the Democratic Republic of the Congo (DRC). (en)
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| - The Kibaran orogeny is a term that has been used for a series of orogenic events, in what is now Africa, that began in the Mesoproterozoic, around 1400 Ma and continued until around 1000 Ma when the supercontinent Rodinia was assembled.The term "Kibaran" has often been used for any orogenic rocks formed during this very extended period.Recently, it has been proposed that the term should be used in a much narrower sense for an event around 1375 Ma and a region in the southeast of the Democratic Republic of the Congo (DRC). These orogenic events are also known as the Grenville orogeny in North America and the Dalslandian orogeny in Western Europe. (en)
- Кібарська складчастість — корелює з дальсландською складчастістю. Кібарська складчастість проявлена в Африці. Гірські породи Кібарської складчастості мають абсолютний вік близько 1 млрд років. Шуберт і Фор-Мюре (1967) зіставляють кібарську складчастість та Ірумідську складчастість з дальсландською і гренвільською, датуючи їх абсолютний вік відповідно 1000 і 900 млн років. (uk)
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