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成矿过程是成矿物质的运动过程，有用元素的活化、迁移、稳定和集中，与“同成矿构造体系”活动时期地应力和能量的集中和构造发生时的释放息息相关。地应力和能量逐步积累，伴随地温升高和水分的参与，促使元素活化，地应力积累到一定程度导致地壳岩石变形、破碎和位移，又引起应力和能量的释放，活化了的元素便向应力降低的构造带集中从而形成矿床。全息光弹和数学模拟可以定量地计算出成矿时区域及矿田中应力和能量的分布状态及其变化，根据应力和能量的高值区与矿化集中的位置关系，可进一步确定矿脉中的富矿段，预测隐伏矿脉的位置，使矿的预测由定性提到定量的高度。
Mineralization is the process of ore-forming material movement. The activation, migration, stabilization and concentration of useful elements are closely related to the concentration of earth stress and energy and the release of tectonism during the syntectonic tectonic activity. The gradual accumulation of in-situ stress and energy, with the increase of ground temperature and the participation of moisture, promote the activation of elements. The accumulation of in-situ stress leads to deformation, crushing and displacement of crustal rocks and the release of stress and energy. The activated elements Stress-reduced tectonic belts concentrate to form deposits. Holographic photoelasticity and mathematical simulation can quantitatively calculate the distribution and changes of stress and energy in the ore-forming area and the ore field. According to the positional relationship between the high value area and the mineralization concentration of stress and energy, it can be further determined The section of the rich ore, which predicts the location of the hidden veins, allows the prediction of the mine to refer qualitatively to the quantitative heights.