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通过对滇西实验场区跨断层短基线、短水准测量的计算分析表明：１９９６年２月丽江７０级地震前，滇西实验场区５个跨断层短基线、短水准测量的测点中，只有位于程海断裂带上的永胜测点（震中距８２ｋｍ）在震前１年左右出现巨变异常，而距震中最近的丽江测点（震中距４２ｋｍ），震前并没有显著的异常变化，但却有很大的同震变化。其它３个测点看不出与该次地震有明显联系的变化。尝试性地进行了两种计算，可能对孕震地区的判断有一定的参考价值。
Through the calculation and analysis of the short baseline and short leveling measurements of the cross-fault in the western Yunnan test area, it is shown that before the July 7.0 Lijiang earthquake, the five short-baseline and short-leveling measuring points , Only the Yongsheng measuring point (epicentral distance 82km) located on the Chenghai fault zone experienced a catastrophic anomaly about 1 year before the earthquake. However, there was no significant anomaly before the earthquake in Lijiang (the epicentral distance of 42km) Change, but there is a great coseismic change. The other three measuring points do not show any obvious changes in connection with the earthquake. Tentatively carried out two kinds of calculations may have some reference value for the judgment of pregnant earthquake area.