小秦岭地体中的褶皱包括露头褶皱和宏观褶皱，组成褶皱的面理为次生构造面理。
The fold in the Xiaoqinling terrane included the outcrop fold and macrofold, and the foliation formed by the fold was the secondary structural foliation.
因此，江南隆起带褶皱基底这一宏观变形强烈、微观变形甚弱的现象属于低温下准塑性变形结果。
The phenomenon of high macroscopic deformation and low microcosmic deformation of the folded basement in the Jiangnan uplift is attributed to the quasi-plastic deformation at low temperatures.
强烈的片理、拉伸线理、a型褶皱、鞘褶皱以及糜棱岩，这些构造特征仅仅反映出宏观的证据。
Strong foliation, stretching lineation, a-type folds, sheath folds and mylonite, these structural characteristics only reflect macroscopic evidence.
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