Coupled stable chromium and iron isotopic fractionation tracing magmatic mineral crystallization in Archean komatiite-tholeiite suites-Reference-Cited by-同舟云学术

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Coupled stable chromium and iron isotopic fractionation tracing magmatic mineral crystallization in Archean komatiite-tholeiite suites

Published:2021-08 Issue: Volume:576 Page:120121
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Wagner Luise J.,Kleinhanns Ilka C.,Weber Nadja,Babechuk Michael G.,Hofmann Axel,Schoenberg Ronny

Funder

German Research Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference166 articles.

1. Modern rather than Mesoarchaean oxidative weathering responsible for the heavy stable Cr isotopic signatures of the 2.95 Ga old Ijzermijn iron formation (South Africa);Albut;Geochim. Cosmochim. Acta,2018

2. Crystal structure of a Cr-2+−bearing pyroxene;Angel;Am. Mineral.,1989

3. The stratigraphy of the 3.5–3.2 Ga Barberton Greenstone Belt revisited: a single zircon ion microprobe study;Armstrong;Earth Planet. Sci. Lett.,1990

4. Differentiation of komatiite flows;Arndt;J. Petrol.,1986

5. Stable and metastable pyroxene crystallization in layered komatiite lava flows;Arndt;Am. Mineral.,1979

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