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层状铜矿床的研究历来受到地质工作者的重视,并已划分为明显受火山作用控制的和明显受沉积作用控制的两个层状铜矿类型.前者称为火山岩型铜矿*或黄铁矿型铜矿,后者称为沉积岩型铜矿或砂(页)岩型铜矿.文献表明,对于成矿既受火山作用影响,又受沉积作用控制,并不同程度地受到区域变质作用改造的层状铜矿,相比之下,没有得到正确对待.它们往往不是被作为火山岩型铜矿,就是被归入砂(页)岩型铜矿,也经常地被认为是岩浆期后的热液型铜矿床(中-高温细脉浸染层状铜矿、中-低温白云岩层状铜矿).
The study of stratiform copper deposits has always been valued by geologists and has been divided into two stratiform copper types that are obviously controlled by volcanism and obviously controlled by sedimentation. The former is called volcanic copper ore * or yellow The latter is called a sedimentary-type copper deposit or a sand-type (copper) type copper deposit. The literature shows that both mineralization is affected by volcanism and controlled by sedimentation and is affected to a different extent by regional metamorphism The altered stratiform copper mine, in contrast, is not properly treated and is often classified not as a volcanic type copper mine, or as a sandstone (copper) type of copper deposit, but is also often thought to be post-magmatic Hydrothermal copper deposit (medium-high temperature vein disseminated stratiform copper deposit, medium-low temperature dolomite stratiform copper deposit).