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东升庙硫－多金属矿床狼山群二组含矿地层中，除已发现的变质石英角斑岩之外，又找到具有变余斑状结构（斑晶主要为钠质斜长石，另有少量辉石和角闪石）的变质基性火山岩和变质凝灰岩夹层以及火山岩屑与晶屑。这既直接证实本矿在成岩成矿期有明显的间歇性火山喷发活动、成矿与火山喷发作用有关，又可为研究本矿床成矿地质构造背景、成岩成矿历史，进而判别矿区古火山口的位置，进行区域对比与确认同生断层等问题提供岩石学的基本素材。此外，它们还可作为本区有效的找矿标志
Among the two ore-bearing strata of the Wolfshan Group in the Dongshengmiao sulfur-polymetallic deposit, besides the metamorphic quartz porphyry that has been found, it has been found that the porphyritic structure is mainly composed of plagioclase platyclair with a small amount of plagioclase Pyroxene and hornblende) metamorphic basement volcanic rocks and metamorphic tuff intercalations as well as volcanic rock debris and crystal debris. This not only directly confirms the mine in the diagenetic mineralization significant intermittent volcanic eruptions, mineralization and volcanic eruptions, but also for the study of the mineralization geological structure background, diagenesis and mineralization, and then identify the ancient volcano The location of the mouth, the regional contrast and confirm the same fault and other issues provide the basic material of petrology. In addition, they can also be used as effective prospecting signs in this area