Laboratory measurements of mineral deformation, change in rheological behavior of rocks with depth and seismic sounding data all show jelly sandwich-like strength envelopes of the continental lithosphere. 矿物变形的实验室研究结果、岩石流变学性质随深度改变和地震测深剖面资料都提示大陆岩石圈具有三明治式的强度包络面。