以水位为主的水动力学效应反映了大区域应力调整过程具有不可逆特征。
The effect of dynamics which mainly is the water level reflected the consolidation process of the big region stress. And it has an irreversible characteristic.
利用赣南地区的基础地质资料，分析了该区域在大受力背景下的应力调整方式。
Based on the geological structure in the south of Jiangxi, this paper has analyzed the stress adjustment mode in that area under the geological background press.
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