利用一种模式可能综合两种端员模式种类（齿状作用和地幔俯冲作用）。这两种端员模式已经用于解释大陆碰撞期间地壳变形作用的模型，这种模式包括了来自侧翼的锯齿模式以及来自于下伏的俯冲层段的底部力作用。沿走向测定变形作用的宽度，可以指示主应力形成机制及受控的情况。如果地壳与下伏的地幔岩石圈吻合良好，可以由地幔俯冲作用控制，或者如果地壳和地幔岩石圈分离，则受控于锯齿状作用。重力对于地壳增厚作用的影响造成变形作用的宽度随着聚敛程度的增加而增加，由此可以形成从地幔俯冲作用到锯齿作用的造山体系的主要控制因素；这种转换可以由变厚的地壳底部的扩散作用或者对流热作用而加强。印度—欧亚碰撞作用是一个实例，那里变形作用宽度最初取决于地幔的俯冲作用，但是现在受锯齿状界线的控制 With one model it is possible to combine two types of endmember modes (dentate and mantle subduction). Both endmember models have been used to model the crustal deformation during the continental collision, including the sawtooth pattern from the flanks and the bottom force from the underlying subduction zone. Determine the width of the deformation along the trend, you can indicate the main stress formation mechanism and controlled conditions. If the crust is well matched with the underlying mantle lithosphere, it can be controlled by mantle subduction or controlled by serration if the crust and mantle lithosphere are separated. The effect of gravity on crustal thickening increases the width of the deformation as the degree of convergence increases, which can form the major controlling factor for the orogenic system from mantle subduction to serration; this conversion can be dominated by thickening crust The bottom of the diffusion or convection heat and strengthen. The Indian-Eurasian collision is an example where the width of deformation is initially dependent on the subduction of the mantle but is now controlled by a jagged boundary