Geochemistry and sedimentology of a facies transition — from microbanded to granular iron-formation — in the early Proterozoic Transvaal Supergroup, South Africa-Reference-Cited by-同舟云学术

Geochemistry and sedimentology of a facies transition — from microbanded to granular iron-formation — in the early Proterozoic Transvaal Supergroup, South Africa

Published:1990-04 Issue:1-2 Volume:47 Page:99-139
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Beukes Nicolas J.,Klein Cornelis

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference45 articles.

1. Microscale chemical effects of low temperature alteration of DSDP basaltic glasses;Ailin-Pyzik;J. Geophys. Res,1981

2. Solar-system abundances of the elements;Anders;Geochim. Cosmochim. Acta,1982

3. Geochronological studies on Archean and Proterozoic formations of the foreland of the Nemaqualand front and possible correlates on the Kaapvaal craton;Armstrong,1987

4. The Krivoy Rog Basin, 211–251;Belevtsev,1983

5. Precambrian iron-formations of southern Africa;Beukes;Econ. Geol,1973

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