结果：基底段到心尖段应变与应变率呈下降趋势，但统计学差异无显著性。
Results: Although strain and strain rate declined from basal segment to apex, there was no statistical difference.
结论：应变与应变率在同一室壁不同节段与不同室壁同名节段之间差异无显著性。
Conclusion: There was no statistical difference of strain and strain rate between the different segments and the different walls.
强震通常发生在剪切应变率的高值区及其边缘，尤其是与构造变形背景相一致的剪应变率高值区。
Strong earthquakes occurred in the high-value region and its margins of shear strain rate, especially in the high-value region of shear strain rate in accordance with tectonic deformation background.
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