The kinematic vorticity number (W_K), which is introduced into geology from fluid dynamics, is used to measure the degree of non-coaxiality of strain.
运动学涡度是从流体力学引入到地质学当中的，主要应用于应变非共轴程度的确定。
The kinematic vorticity number (W_K), which is introduced into geology from fluid dynamics, is used to measure the degree of non-coaxiality of strain.
运动学涡度是从流体力学引入到地质学当中的，主要应用于应变非共轴程度的确定。
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