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通过对已知矿床不同级序的地质、地球化学和地球物理等客观属性的分析，研究了冀北地区铅锌银矿床成矿的地质要素．认为成矿地质属性在时空结构上具有一定匹配和耦合规律，前寒武纪和中新生代地质作用在空间上的耦合，与不同尺度的接触带构造在时间上的匹配，构成了四维时空格架：从矿床～矿带～成矿区，成矿地质要素分别是接触带构造、中生代构造一岩浆活动带和前寒武纪结晶基底
Based on the analysis of geochemical, geochemical and geophysical properties of different orders of known ore deposits, the geological elements of metallogenic lead-zinc-silver deposits in northern Hebei were studied. It is considered that the geological properties of ore-forming have some matching and coupling rules in the space-time structure. The spatial coupling between the Precambrian and Meso-Cenozoic geologic functions in time matches with the contact structure at different scales, forming a four-dimensional space-time lattice Frames: From ore deposits to mineralization areas, the ore-forming geological elements are the contact belt structure, the Mesozoic tectonic-magmatic belt and the Precambrian crystalline basement