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秦岭造山带核部杂岩即秦岭杂岩南北两侧商丹、朱夏边界剪切带逆－左行和逆（正）－右行相配套的剪切、杂岩内部广泛发育的东倾的Ａ型构造、变质作用的近等温降压以及花岗岩体侵位中心的向东偏移的特点揭示，该杂岩相对两侧古生代地层发生过（晚加里东－早海西期）向西的平行造山带的侧向运移、抬升；水平相对位移量约３２－８６ｋｍ：垂向相对抬升量约为１５－４０ｋｍ：其动力学背景是杂岩两侧盆地由东向西剪刀状双向俯冲闭合造成的侧向挤出。
The Qinling orogenic belt nuclear complex that is, Qinling Shendan on both sides of the North and South Shangdan, Zhuxia boundary shear zone reverse - left and reverse (positive) - right line of the matching shear, the extensive development of the eastern interior of the A Type tectonics, near-isothermal depressurization of metamorphism and an eastward shift of the emplacement center of the granite body reveal that the Paleozoic strata on opposite sides of the complex (Late Caledonian-Early Hercynian) The lateral displacement of the belt is about 32-86km: the vertical relative lift is about 15-40km: its dynamic background is caused by the scissors-like two-way subduction closure on both sides of the complex in the basin Lateral extrusion.