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本文概述了苏联近年来在矿田和矿床构造研究上的某些新动向。如强调用构造分析来查明矿化富集条件和探讨矿床成因;显微构造分析用于定性评价控矿构造形成的温压条件和划分矿田断裂动力影响区和动力变质带;利用测定岩、矿石传播弹性波速度的方法来研究控矿构造,恢复成矿构造应力场和查明岩浆岩的形成深度;通过测定岩石的物理力学性质,计算岩石综合物理系数,从而近似定量评价岩石在成矿过程中的性质和作用。
This article summarizes some of the recent developments in the field of ore deposits and mineral deposits in the Soviet Union. Such as emphasizing the use of tectonic analysis to ascertain the mineralization enrichment conditions and explore the genesis of the deposit; microstructural analysis is used to qualitatively evaluate the temperature and pressure conditions for the formation of ore-controlling structures and to divide the dynamic influence zones and dynamic metamorphic zones of the orefield; , Ore propagation elastic wave velocity method to study the structure of ore control, restoration of metallogenic tectonic stress field and to ascertain the depth of formation of magmatic rocks; by measuring the physical and mechanical properties of rock, calculate the rock physical coefficient, and thus quantitatively approximate the rock in The nature and role of the mine process.