... Amoeboid protozoans 阿米巴状原生动物 amoeboid fold 变形褶皱 Amoeboid Changeling 阿米巴化形 ...
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风成沙丘普遍存在角砾前积、拖曳褶皱和倒转褶皱等同沉积变形构造。
The synsedimentary deformation structures are common in eolian dunes, such as brecciated foresets, drag folds and overturned folds.
根据变形力的强度，褶皱可以是平缓的，陡峭的，倒转的，或逆掩的。
Depending on the intensity of the deforming forces the folds may be gentle sharp overturned or overthrust.
中期是地块的最终固结阶段，在此期间发生了褶皱变形，是高压变质作用的初期阶段；
The middle stage witnesses final consolidation of the massifs, their participation in fold deformations, which coincide with the initial stages of high P metamorphism.
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