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国内外学者对崆岭群的研究已有悠久的历史。早在1907年,Blackwelder认为鄂西崆岭层(群)相当泰山式(群)的基底杂岩。李四光等于1924年在长江峡东地区工作后,把峡东前震旦系变质岩称为“三斗坪系”(分成崆岭片岩、美人沱片麻岩和黄陵花岗岩)。1958年,北京地质学院在黄陵背斜进行一比二十万区测工作,将该区变质岩系称为崆岭群,并进行了地层划分。1959年,全国地质会议根据地质部水文工程地质队在该区侵入岩——英闪岩的耳个同位素年龄样,推测岩浆岩与片岩发生混合作用的时代为800—900
Scholars at home and abroad have a long history of research on Yu Ling Group. As early as 1907, Blackwelder thought that the West Tieling layer (group) of western Hubei is quite Taishan type (group) basement complex. After Li Siguang was equal to working in the Yangtze River Gap East in 1924, he called the former East Sinian metamorphic rock “Sandouping” (divided into the Juling schist, the Mei Ren Tuo gneiss and the Huangling granite). In 1958, Beijing Institute of Geology conducted a survey of one to two hundred thousand zones in the Huangling anticline, calling the metamorphic series in the area a Geling Group and stratigraphic division. In 1959, according to the ear isotopic ages of the intrusive rocks and amphibolite from the geologic hydrology engineering geology team in the area, the National Geological Conference speculated that the mixing time of magmatic rocks and schists was 800-900