Their features and development are markedly different form those of Alpine-type nappe found in geosynclinal-folded belts.
其地质背景特征与发育于地糟褶皱带的阿尔卑斯式推覆构造有明显的差别。
Their features and development are markedly different form those of Alpine-type nappe found in geosynclinal-folded belts.
其地质背景特征与发育于地糟褶皱带的阿尔卑斯式推覆构造有明显的差别。
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