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• W2067321927 abstract "Mechanical weakening due to solid state transformation of mineral phases has long been proposed to be a significant mechanism for localization of deformation in the Earth’s lithosphere and the mantle transition zone. However, experimental observations confirming such a proposition are lacking. Here we present a novel approach to prove the existence of a minimum in the creep strength of quartz at the α–β transition by observing the deformation of fluid inclusions in a quartz crystal using a hydrothermal diamond-anvil cell. Pressure differences required for permanent deformation of the quartz around fluid inclusions were significantly lower at the phase transition than in either the stability fields of α- or β-quartz. These results indicate that transformation plasticity of silicates can indeed cause a considerable localized reduction in the strength of the Earth’s crust and mantle." @default.
• W2067321927 created "2016-06-24" @default.
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• W2067321927 date "2003-01-01" @default.
• W2067321927 modified "2023-10-10" @default.
• W2067321927 title "Experimental evidence of transformation plasticity in silicates: minimum of creep strength in quartz" @default.
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• W2067321927 doi "https://doi.org/10.1016/s0012-821x(02)01046-4" @default.
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