Carbonate Tuff Cones in Northern Tanganyika-Reference-Cited by-同舟云学术

Carbonate Tuff Cones in Northern Tanganyika

Published:1964-04-17 Issue:2 Volume:101 Page:129-137
ISSN:0016-7568
Container-title:Geological Magazine
language:en
Short-container-title:Geol. Mag.

Author:

Dawson J. B.

Abstract

AbstractThe carbonate matrix of several pyroclastic tuff rings and cones in the Monduli-Arusha area of northern Tanganyika, is believed to be of volcanic carbonatitic origin. One of the pyroclastic tuff rings contains ejected blocks of ultrabasic composition which are minera-logically similar to the cognate xenoliths found in kimberlite pipes.

Publisher

Cambridge University Press (CUP)

Subject

Geology

Reference17 articles.

1. Chilwa Island;Garson;Geol. Surv. Nyasaland,1958

2. Carbonatites in the Rufunsa valley, Feira district;Bailey;Bull. N. Rhod. geol. Surv.,1960

3. Garson M. S. , 1961. The Tundulu carbonatite ring complex in southern Nyasaland. Ph.D. Thesis, Univ. Leeds.

4. The alkaline district of Alno Island;Eckermann;Sver. Geol. Undersok.,1948

5. Dawson J. B. , 1960. A comparative study of the geology and petrography of the kimberlites of the Basutoland province. Ph.D. thesis, Univ. Leeds.

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