Iron isotopic evolution during fractional crystallization of the uppermost Bushveld Complex layered mafic intrusion-Reference-Cited by-同舟云学术

Iron isotopic evolution during fractional crystallization of the uppermost Bushveld Complex layered mafic intrusion

Published:2017-03 Issue:3 Volume:18 Page:956-972
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Bilenker Laura D.¹²^ORCID,VanTongeren Jill A.³,Lundstrom Craig C.⁴^ORCID,Simon Adam C.¹

Affiliation:

1. Department of Earth and Environmental Sciences; University of Michigan; Ann Arbor Michigan USA

2. Now at Department of Earth, Ocean, and Atmospheric Sciences, Pacific Centre for Isotopic and Geochemical Research; University of British Columbia; Vancouver BC V6T 1Z4 Canada

3. Department of Earth and Planetary Sciences; Rutgers University; Wright Geological Laboratory 343 Piscataway New Jersey USA

4. Department of Geology; University of Illinois; Champaign Illinois USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016GC006660/fullpdf

Reference48 articles.

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2. Variations in Cr content of magnetite from the upper zone of the Bushveld complex: Evidence for heterogeneity and convection currents in magma chambers;Cawthorn;Earth Planet. Sci. Lett.,1980

3. Iron isotope fractionation during crystallization and sub-solidus re-equilibration: Constraints from the Baima mafic layered intrusion, SW China;Chen;Chem. Geol.,2014

4. Iron isotopic compositions of geological reference materials and chondrites;Craddock;Geostand. Geoanal. Res.,2011

5. Iron isotopes may reveal the redox conditions of mantle melting from Archean to present;Dauphas;Earth Planet. Sci. Lett.,2009

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