Jin-Qu Basin is situated at the junction of west-Zhejiang Qiantang syncline and east-Zhejiang folded zone.
金衢盆地发育于浙西钱塘台拗和浙东华夏褶皱带接洽部位，受北东向和东西向断裂联合制约。
Pre—Bogda mountain folded zone is one of the most complicate and grand tectonic unit at pre—mountain area in China.
博格达山前褶皱带是我国最复杂、最雄伟的山前构造单元之一。
Garze-Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.
甘孜-理塘断裂带是义敦造山带与雅江褶皱带的分界断裂。
Garze-Litang fracture zone separates Yidun orogenic belt from Yajiang folded belt.
甘孜-理塘断裂带是义敦造山带与雅江褶皱带的分界断裂。
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