为了简化地质构造力学分析,本文探讨了用内力线来描绘应力场的方法。
For the sake of simplifying the analysis of geological structural mechanics, the method using endogenetic force lines in the description of the stress fields is advanced in this paper.
平卧褶皱若未经后来构造变动,其图面特征与水平地层区完全一样,除了褶皱转折端以外,只是一系列平行等高线的地质界线。
Without late tectonic deformation, the features of recumbent fold on the geological map would be the same as those of horizontal strata.
本文阐述在断裂构造地质地带的公路定线问题。
This paper investigates the highway alignment in the fault structural zone.
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