imbricate thrusting

基本解釋

The middle(early Himalayan)is the main deformation, characterized by the imbricate thrust structure system, whose west zone shows thrusting from SW toward NE.
中期（喜馬拉雅早期）是主變形期，西帶顯示由SW向NE逆沖，以疊瓦狀逆沖構(gòu)造系統(tǒng)為其特征。
From north to south, several tectonic belts can be distinguished:front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.
由北向南分為前緣擠壓滑脫構(gòu)造帶、斜歪倒轉(zhuǎn)褶皺—逆沖斷層帶和逆沖推覆巖席及疊瓦狀逆沖斷層帶。