Fluid-assisted strain localization in the shallow subcontinental lithospheric mantle
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文摘

Evidence for a feedback between fluid flow and strain localization in the shallow mantle.

Microstructural evidence for fluid-assisted dissolution–precipitation in peridotites.

Olivine CPO in mylonites indicates (001)[100] glide, probably in presence of fluids.

Evolution from dislocation creep to dissolution–precipitation by fluid focusing.

Abnormal orthopyroxene CPO interpreted as due to oriented crystallization.

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