1·Thedetermined structural deformation features through systematic tracing the marker bed in the area are geologically significant to correctly recognizing the formation and evolution of the orogen.
通过对区内标志岩层组合的系统追索，所确定的构造变形特征，对正确认识该造山带的形成演化具有重要地质意义。
2·Taihangshan orogen, called tectonomagmatic belt by most of geologists, is thought to be a part of Mesozoic circum Pacific magmatic arc.
太行山造山带被大多数学者称为构造岩浆带，被认为是中生代环太平洋岩浆弧的组成部分。
3·Continental crust chemical structure of Qinling-Dabie Orogen.
秦岭-大别造山带地壳化学结构。
4·Such structure in the collision foredeep of the Dabieshan Orogen was resulted in inelastic extensional deformation of the conver side of the flexed plate aroused by lithospheric flexure.
这些伸展构造很显然是扬子克拉通和华北克拉通在三叠纪碰撞时，大别山造山带前陆位置岩石圈弯曲导致地壳上部产生非弹性变形的结果。
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。