The Result of Tangential Layered Solid-State Flow Deformation in the Middle and Lower Crust: the Yardoi Dome in the Eastern Himalayan Orogenic Belt
ACTA PETROLOGICA SINICA（2024）
Key words
Yardoi gneiss dome,South Tibet,Formation mechanism of gneiss dome,Layered solid-state flow deformation,Middle and lower crust,Strain rate,Kinematic vorticity
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