{"title":"刚果人民共和国的年表","authors":"Pierre Gioan, Jean-Paul Vicat","doi":"10.1016/0899-5362(87)90062-5","DOIUrl":null,"url":null,"abstract":"<div><p>Comprehensive measures of radiometric age have been made on proterozoic rock samples belonging to various structural units in the People's Republic of the Congo (Mayumbian belt, Niari synclinorium, Sembé-Ouesso sequences). Having gathered them in tables, we have been able to date certain major tectonic events. The calc-alkalic magmatism associated with the Mayumbian belt (1400 Ma) is linked to the oceanic closure (Kibarian orogenesis) and the ultimate metamorphic episode is dated at 600 Ma (Pan-African). The Niari synclinorium sedimentary sequences, which were deposited from 1000 Ma on, have undergone Pan-African metamorphism. Moreover, we notice a systematic rejuvenation attributed to the South Atlantic proto ocean opening. At last, the Sembe-Ouesso sequences have been subjected to an epimetamorphic episode around 630 Ma, probably also linked to the Pan-African orogenesis.</p></div>","PeriodicalId":100749,"journal":{"name":"Journal of African Earth Sciences (1983)","volume":"6 2","pages":"Pages 215-220"},"PeriodicalIF":0.0000,"publicationDate":"1987-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0899-5362(87)90062-5","citationCount":"5","resultStr":"{\"title\":\"Bilan géochronologique de la République Populaire du Congo\",\"authors\":\"Pierre Gioan, Jean-Paul Vicat\",\"doi\":\"10.1016/0899-5362(87)90062-5\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Comprehensive measures of radiometric age have been made on proterozoic rock samples belonging to various structural units in the People's Republic of the Congo (Mayumbian belt, Niari synclinorium, Sembé-Ouesso sequences). Having gathered them in tables, we have been able to date certain major tectonic events. The calc-alkalic magmatism associated with the Mayumbian belt (1400 Ma) is linked to the oceanic closure (Kibarian orogenesis) and the ultimate metamorphic episode is dated at 600 Ma (Pan-African). The Niari synclinorium sedimentary sequences, which were deposited from 1000 Ma on, have undergone Pan-African metamorphism. Moreover, we notice a systematic rejuvenation attributed to the South Atlantic proto ocean opening. At last, the Sembe-Ouesso sequences have been subjected to an epimetamorphic episode around 630 Ma, probably also linked to the Pan-African orogenesis.</p></div>\",\"PeriodicalId\":100749,\"journal\":{\"name\":\"Journal of African Earth Sciences (1983)\",\"volume\":\"6 2\",\"pages\":\"Pages 215-220\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1987-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0899-5362(87)90062-5\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of African Earth Sciences (1983)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0899536287900625\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of African Earth Sciences (1983)","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0899536287900625","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Bilan géochronologique de la République Populaire du Congo
Comprehensive measures of radiometric age have been made on proterozoic rock samples belonging to various structural units in the People's Republic of the Congo (Mayumbian belt, Niari synclinorium, Sembé-Ouesso sequences). Having gathered them in tables, we have been able to date certain major tectonic events. The calc-alkalic magmatism associated with the Mayumbian belt (1400 Ma) is linked to the oceanic closure (Kibarian orogenesis) and the ultimate metamorphic episode is dated at 600 Ma (Pan-African). The Niari synclinorium sedimentary sequences, which were deposited from 1000 Ma on, have undergone Pan-African metamorphism. Moreover, we notice a systematic rejuvenation attributed to the South Atlantic proto ocean opening. At last, the Sembe-Ouesso sequences have been subjected to an epimetamorphic episode around 630 Ma, probably also linked to the Pan-African orogenesis.
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