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以聚铀过程为例，对成矿系统运用耗散结构理论进行初步探讨。结果表明：（１）成矿系统是一个非平衡、自组织的开放系统，具非线性叠加性和高度有序性；（２）地质力是聚铀过程中导致负熵演化的动力来源；（３）构造运动及其多旋回性是成矿系统演化并产生新质变、新量变的巨涨落；（４）聚矿系统的耗散结构可由数学模型进行归纳。
Taking the process of poly uranium as an example, a preliminary discussion is made on the application of dissipative structure theory to metallogenic systems. The results show that: (1) the ore-forming system is an unbalanced and self-organizing open system with non-linearity and highly orderliness; (2) the geologic force is the source of negative entropy evolution in poly-uranium; 3) tectonic movement and its multi-cycle are the evolution of the metallogenic system and the generation of new qualitative changes, the new quantitative change of the huge fluctuations; (4) the melting system of the dissipative structure can be summarized by the mathematical model.