1·Continental crust chemical structure of Qinling-Dabie Orogen.
秦岭-大别造山带地壳化学结构。
2·Jurassic; Micang Shan; Sichuan basin; Qinling; basin-orogen coupling.
侏罗系；米仓山；四川盆地；秦岭；盆山耦合。
3·So Wedging was the mechanism for mountain building in the Qinling orogen.
楔入构造活动是秦岭造山带的成山模型。
4·Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
5·Detrital composition analysis of the Mesozoic sandstones indicates that their provenance is the Dabie orogen.
中生界砂岩碎屑组分分析，表明其源区为大别造山带。
6·Although the study on the orogen has been continuing for about 100 years, it is still the hotspot in geology.
造山带虽然经过近代一百多年的研究，但仍一直是地质科学研究的前沿课题。
7·The tectonic composition and evolutionary history of this orogen are also discussed in the meantime in this paper.
同时讨论了这个造山带的结构组成和演化历史；
8·Being an important pluton in the western part of Altay orogen, Tielieke pluton shows arc granitoid characteristics.
铁列克岩体是阿尔泰造山带西段的一个重要的岩体，显示弧花岗岩特征，其侵位时代一直没有解决。
9·Sediments in the Hefei basin to the north of the Dabie orogen are important records of unroofing history for the orogen.
位于大别造山带北部的合肥盆地，其中的沉积是造山带剥露历史的重要记录。
10·Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。