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若先行假设一个区域应力系统,使其最大主压方向平行于岩墙型式的对称线,并且将其迭加在局部应力系统以上,那末,根据应力分析就可以解释科罗拉多州西班牙山周围形态奇特的岩墙型式了。西班牙山侵入物质的静压产生了本区的局部应力系统。为简化计算起见,假定了一个圆孔位于西班牙山的西峰。西班牙山以西的山前带,规定出未知的边界条件,若通过假设一想象来源来描述它,能得到圆满的结果。在安迪生(1951,第3章)所提出的应力场与岩墙型式关系的假定基础上,就有可能计算出岩墙型式,这种计算出的岩墙型式在许多方面与所观测的岩墙型式是相符的。
If we first assume that a regional stress system is such that its maximum principal pressure is parallel to the line of the dyke wall and superimposes it above the local stress system, then stress analysis can explain the strange shapes around the Spanish mountains of Colorado Rock wall type. The hydrostatic pressure of intrusions in the mountains of Spain creates a local stress system in this area. To simplify the calculation, assume a circular hole located in the Spanish Peak Xifeng. The piedmont belt west of Spain, which sets out the unknown boundary conditions, can yield satisfactory results if it is described by assuming an imaginative source. Based on the assumptions made by Andy (1951, Chapter 3) about the relationship between the stress field and the type of dyke, it is possible to calculate the type of dyke, which is in many ways related to the observed rock The wall pattern is consistent.