糜棱岩定向标本研究表明，构造带中韧性变形具有右行剪切特征；
The orientation of mylonites indicates that the ductile deformation is of right-hand shearing character in KSTB.
下一步我们应该在韧性剪切带中采集一系列的定向标本，通过室内的显微组构实验研究，我们将获取更多的证据。
What should we do next is to collect a series of oriented samples in the ductile shear zone. We will get more evidence through the indoor experiment work of microfabric study.
下一步我们应该在韧性剪切带中采集一系列的定向标本，通过室内的显微组构实验研究，我们将获取更多的证据。
What should we do next is to collect a series of oriented samples in the ductile shear zone. We will get more evidence through the indoor experiment work of microfabric study.
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