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赣东北多期造山带发育一种双层复合逆冲推覆构造，它是由下部的登山—横峰逆冲断层系和上部的葛源逆冲推覆构造共同构成。地质年代学及运动学研究表明，登山—横峰逆冲断层系形成于加里东期，自南东向北西运移达３０ｋｍ以上，应变速率ε＝２．４×１０－１２／ｓ。葛源逆冲推覆构造则形成于印支期，自北西向南东运移至少５０ｋｍ。
A multi-phase orogeny thrust nappe structure developed in the multi-period orogen of northeastern Jiangxi Province consists of the lower mountaineering-Hengfeng thrust fault system and the upper Geyuan thrust nappe structure. Geochronology and kinematics studies show that the mountaineering-Hengfeng thrust system was formed in the Caledonian Period and migrated from south to east to north and west for more than 30km with a strain rate of ε = 2.4 × 10-12 / s. Ge source thrust nappe structure was formed in the Indosinian period, from northwest to southeast migration at least 50km.