无论是原生的还是次生的矿床,其周围的分带模式都是制定大多数探矿计划的依据。最普通的矿床主岩的原生分带模式的最重要的表现是,矿石、脉石或围岩蚀变中的矿物变化和矿体或围岩中的元素丰度变化。通常很少看到流体包体的温度和成分的分带模式。虽然近来对一些斑岩铜矿和大型硫化物矿床的研究已证明,较大的更复杂的系统显示出大规模的原生分带模式,这就大大地扩大了勘探目标,但对矿床周围分带模式的大部分研究工作还是集中 Whether in primary or secondary deposits, the zoning pattern around them is the basis for most prospecting plans. The most common manifestation of the most common primary zonation pattern of host rocks is the change in mineralogy during mineralization, gangue or wall rock alteration and the elemental abundance in the ore body or surrounding rock. Often it is rare to see the temperature of the fluid inclusions and the zonation pattern of the components. Although recent studies of some porphyry copper and large-scale sulfide deposits have shown that larger, more complex systems show large-scale primary zonation patterns, greatly expanding exploration targets, but zoning around the deposit Most of the research work on the model is still focused