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本文据锡矿山区古构造特征,运用相应的岩石破裂理论,对该区成矿期构造应力场进行数学力学的计算,其结果与该区古构造特征吻合得较好,并与国内外其它方法估算的古应力值可以对比。
Based on the paleotectonic features of the tin mines and the corresponding theory of rock failure, the mathematical mechanics of the tectonic stress field during the metallogenic stage is calculated. The results agree well with the palaeo-tectonic features of this area and are in good agreement with other methods The estimated ancient stress values can be compared.