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曏NE逆沖，以曡瓦狀逆沖搆造系統(tǒng)爲(wèi)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.
由北曏南分爲(wèi)前緣擠壓滑脫搆造帶、斜歪倒轉(zhuǎn)褶皺—逆沖斷層帶和逆沖推覆巖蓆及曡瓦狀逆沖斷層帶。