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Journal Article

Climatic oscillations as registered through the Ruzizi Plain deposits (north Lake Tanganyika) Zaire-Burundi-Rwanda

Greenhouse effect, sea level and drought. Proc., workshop, Fuerteventura, 1989 (1990) 287-299
DOI: 10.1007/978-94-009-0701-0_18
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Abstract

The Ruzizi Plain deposits show evidence of alternating savannah and semi-arid cliamtes deduced from geomorphology (calcretes - ferricretes - stone-line), sedimentology (meandering river-braided river-sheetflood deposits), and pedology (Gley-Pseudogley-Alfisol-Calcrete paleosols). -Authors

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APA

Ilunga, L., & Paepe, R. (1990). Climatic oscillations as registered through the Ruzizi Plain deposits (north Lake Tanganyika) Zaire-Burundi-Rwanda. Greenhouse Effect, Sea Level and Drought. Proc., Workshop, Fuerteventura, 1989, 287–299. https://doi.org/10.1007/978-94-009-0701-0_18

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