当我们在多金属及其他矿床进行工作时,往往发现有许多岩墙(各种斑岩、玢岩、煌斑岩、辉绿岩岩墙)与礦脉相互伴生或穿插。时常因未掌握岩墙与礦脉在空间和时间上的分布规律,妨碍了找礦、勘探和开采工作,以及对礦床的正确评价。对岩墙与礦脉的相互关系进行研究;将能指导实际工作,发现许多有意义的事实,并能帮助我们了解目前许多未能解决的理论问题。 When we work in polymetallic and other deposits, we often find many dikes (various porphyry, pluton, lamprophyre, diabase dikes) associated or interlaced with the veins. The failure to grasp the spatial and temporal distribution of dikes and veins often hinder ore prospecting, exploration and exploitation, and correct evaluation of the deposit. Studying the interrelationship between dikes and veins will guide practical work, discover many meaningful facts and help us understand many of the theoretical problems that can not be solved at present.