Abstract:Plagioclase, a major rock‐forming mineral in the Earth's crust, often shows microstructural evidence of ductile deformation in crustal rocks, suggesting that crustal flow is largely controlled by the high‐temperature deformation behavior of this mineral. Here, we present uniaxial and pure shear deformation experiments that reveal various diffusion creep characteristics of anorthite (CaAl2Si2O8), a calcium‐rich plagioclase endmember. We synthesized fine‐grained (∼1 μm) anorthite aggregates with different Al/Si … Show more
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