与地质结果的差异表明，川滇菱形块体的现今地壳运动由北往南逐渐增强；
The results indicate that the crustal movement of the area in north and west are stronger than that of south and east.
川滇应力区东边界（东边的应力转换带）基本上与川滇菱形块体的东边界相吻合；
The eastern boundary of Sichuan-Yunnan stress zone (the eastern stress transition belt) is basically consistent with the eastern boundary of Sichuan-Yunnan rhombic block.
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