岩石分区碎裂化现象是伴随深部岩体的特殊工程响应问题之一。
The phenomenon of zonal disintegration is a special technical problem which comes with deep mass.
深部岩体具有典型的不均匀、不连续的自应力块系等级构造结构。
Deep rock mass has a typical inhomogeneous and discontinuous self-stressed block-hierarchical structure.
研究成果对于深部岩体的热–力耦合特性研究具有一定参考意义。
The results may provide a helpful reference for better understanding the coupled thermo-mechanical behaviors of deep rocks.
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