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利用ＭＤＤ模式得到的连续冷却曲线，可以定量地描述地质体的冷却（隆升）过程；采用我国７个不同地区中３８个钾长石ＭＤＤ模式研究结果证明，快速冷却事件存在的普遍性，不同的快速冷却速度可能反映了不同的构造事件；突变因子（δｖｉ）可以定量地描述地质体非平稳运动以及突变程度，并且使得不同地质事件非平稳程度的对比成为可能
The continuous cooling curve obtained by MDD mode can quantitatively describe the cooling (uplifting) process of the geological body. Using the results of 38 K-feldspar MDD models in seven different areas in China, it is proved that the rapid cooling event exists universality and difference The rapid cooling rate may reflect different tectonic events. The mutation factor (δvi) can quantitatively describe the non-stationary motion of geologic bodies and the degree of abrupt change, and make it possible to compare the non-stationary degree of different geological events