Upon heating the zeolite, the normal siloxane linkage would also experience strain due to thermal expansion.
当加热沸石时，由于热膨胀作用，正常的硅氧烷键也会存在张力。
Particularly, for the continent, the crust thickness, thermal age and strain rate significantly had strong effect on the lithosphere strength.
尤其对于大陆岩石圈，地壳厚度、年龄和应变率均可显著影响岩石圈的强度。
From this reason the creep strain and the thermal expansion can be separately examined and added.
由于这两个性质，蠕应变和热应变可分开研究，而且可线性叠加。
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