2012
DOI: 10.1590/s0370-44672012000400010
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The rheology of banded iron formation: constraints from axial compression experiments

Abstract: . Strain is localized in hematite-rich layers. One intriguing observation is that quartz grains within the more deformed hematite-rich bands show more evidence for crystal-plastic deformation than grains in quartz-rich bands.

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