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依据鲁西地区早前寒武纪花岗质侵入岩普遍具有塑性流变特征和退化变质特征，以及变质作用和变形作用相协调等现象，认为岩体的侵位与变形、变质是同一期构造岩浆作用形成的，是岩浆就位后逐渐冷凝过程中，在持续应力作用下发生的，与后期的地质构造作用无关；固态岩石只能发生脆性变形和局部的脆韧性变形。并从热力场、动力场和化学场的变化趋势对变形、变质作用的制约因素作了简要分析。
Based on the fact that the Early Precambrian granitic intrusions in the Luxi area generally have the characteristics of plastic rheology and degenerated metamorphism and the coordination of metamorphism and deformation, it is considered that the emplacement, deformation and metamorphism of the rock mass are in the same period of tectono-magma The formation of the magma takes place after the magma is in place and gradually condenses, which takes place under the effect of continuous stress, which has nothing to do with the later geological structure. The solid rock can only undergo brittle deformation and local brittleness and ductile deformation. In addition, the restrictive factors of deformation and metamorphism are briefly analyzed from the changing trends of the thermal field, the dynamic field and the chemical field.