Pyrite in a sulfate-poor Paleoarchean basin was derived predominantly from elemental sulfur: Evidence from 3.2 Ga sediments in the Barberton Greenstone Belt, Kaapvaal Craton-Reference-Cited by-同舟云学术

Pyrite in a sulfate-poor Paleoarchean basin was derived predominantly from elemental sulfur: Evidence from 3.2 Ga sediments in the Barberton Greenstone Belt, Kaapvaal Craton

Published:2017-01 Issue: Volume:449 Page:135-146
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Galić Aleksandra,Mason Paul R.D.,Mogollón José M.,Wolthers Mariëtte,Vroon Pieter Z.,Whitehouse Martin J.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference94 articles.

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4. The five stable isotope compositions of Fig Tree barites: Implications on sulfur cycle in ca. 3.2Ga oceans;Bao;Geochim. Cosmochim. Acta,2007

5. Comment on “Early Archaean microorganisms preferred elemental sulfur, not sulfate”;Bao;Science,2008

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