The formation of Palæoproterozoic banded iron formations and their associated Fe and Mn deposits, with reference to the Griqualand West deposits, South Africa-Reference-Cited by-同舟云学术

The formation of Palæoproterozoic banded iron formations and their associated Fe and Mn deposits, with reference to the Griqualand West deposits, South Africa

Published:2000-01 Issue:1 Volume:30 Page:1-24
ISSN:1464-343X
Container-title:Journal of African Earth Sciences
language:en
Short-container-title:Journal of African Earth Sciences

Author:

Klemm Dietrich D.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference101 articles.

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2. Microfossils from the NeoArchæan Campbell Group, Griqualand West Sequence of the Transvaal Supergroup, and their palæoenvironmental and evolutionary implications;Altermann;Precambrian Research,1995

3. The carbonates of the Transvaal and Griqualand West Sequences of the Kaapvaal craton, with special reference to the Lime Acre limestone deposits;Altermann;Mineralium Deposita,1995

4. Limits of the natural environment in terms of pH and oxidationreduction potentials;Baas Becking;Journal Geology,1960

5. Emplacement of a large igneous province as a possible cause of banded iron formation 2.45 billion years ago;Barley;Nature,1997

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