Abstract
THE ages of carbonatites which occur within the Suregei–Asille Volcanics of northern Kenya cannot be obtained at present by directradioisotope dating, but can be derived from the 40Ar/39Ar K–Ar isochron ages of intercalated felsic ignimbrites. The Suregei–Asille Volcanics crop out over an area of some 1,000 km2 to the north-east of Lake Rudolf. They rest unconformably on the Precambrian basement and comprise several volcanic formations. The rock types include flood basalts; Strombolian cinder cones; aa- and pahaoehoe-flows varying in composition from ankaramitic basalt to trachyte; felsic air-fall and ash-flow deposits; lahars; carbonatite volcanics; and a variety of reworked volcanic ashes, volcaniclastic and fluviatile sediments.
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FITCH, F., WATKINS, R. & MILLER, J. Age of a new carbonatite locality in northern Kenya. Nature 254, 581–583 (1975). https://doi.org/10.1038/254581a0
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DOI: https://doi.org/10.1038/254581a0
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