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Ｍüｎｃｈｂｅｒｇ地块是一个角闪岩相变质的结晶基底，构造推覆于极低级变质古生代火山－沉积岩之中．榴辉岩呈透镜状或互层状产于斜长角闪岩、片麻岩和大理岩之中．榴辉岩的原生矿物组合是石榴石、绿辉石、石英和金红石，可含少量蓝晶石、多硅白云母和黝帘石，峰期变质作用的温度为６００～７００℃，压力＞２．５ＧＰａ，接近柯石英的稳定范围．在榴辉岩的抬升过程中经历了从榴辉岩到角闪岩相、绿片岩相和葡萄石绿纤石相退变质作用．退变质作用的早期为近等温降压过程，晚期为降压和快速降温过程．
The Münchberg massif is a amphibolite facies metamorphic crystalline basement that was struck in extremely low-grade Paleozoic volcanic-sedimentary rocks. Eclogites are lenticular or interlayered in amphibolite, gneiss and marble. The primary mineral assemblage of eclogites is garnet, omphacite, quartz and rutile, which can contain a small amount of kyanite, phengite and zoisite. The peak metamorphism temperature is 600 ~ 700 ℃, pressure> 2 .5GPa, close to the stable range of coesite. During the uplift of the eclogite, the metamorphism of the eclogites to the amphibolite facies, the greenschist facies and the gravel greenstone was experienced. The early degeneration of the role of nearly isothermal blood pressure process, the late step-down and rapid cooling process.