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大别山的石英硬玉岩是大别山超高压变质杂岩中的重要成员，与大理岩和榴辉岩紧密共生，呈大小不等的构造透镜体产出在云母斜长片麻岩和含硬玉片麻岩中，分布在长约４０ｋｍ，宽约１ｋｍ的带内。透镜体中心常为花岗变晶结构，边部有不同程度退变并面理化，向外围逐渐变为含硬玉片麻岩。岩石的主要矿物组成为硬玉、石英、石榴石、金红石。退变的石英硬玉岩中还有钠长石、霓石、霓辉石、榍石等。硬玉和石榴石中都有柯石英包体。硬玉的Ｊｄ端元组分为８１．２５％～９０．２７％。恢复的石英硬玉岩的原岩为硬砂岩，与大理岩伴生的榴辉岩的原岩为泥灰岩。因此，石英硬玉岩与共生的大理岩和榴辉岩都属于榴辉岩相变质的表壳岩系，它的成带分布、其中有柯石英的产出，进一步证明大陆地壳能够俯冲到１００ｋｍ左右深度并迅速折返地壳后使其中的高压标志保存完好。
Dabieshan quartz jadeite is an important member of the UHP metamorphic complex in the Dabie Mountains and closely interbedded with marble and eclogite, and structural lenses with unequal sizes are produced in mica plagioclase gneiss and jadeite-bearing gneiss In the distribution of the length of about 40km, width of about 1km band. The center of the lens is often granite crystal structure, with varying degrees of edge degeneration and physicalization, to the periphery gradually become hard jade gneiss. The main rock mineral composition of jade, quartz, garnet, rutile. Degraded quartz jadeite also albite, aegirine, ni-ray stone, stone and so on. Both jadeite and garnet have coesite inclusions. Jade Jade end Jupite component of 81.25% to 90.27%. The original rock of the recovered quartz jadeite is hard sandstone, while the original rock of the eclogite associated with the marble is marl. Therefore, quartz jadeite and symbiotic marble and eclogite belong to eclogitic metamorphic crustal rocks, and their belt distribution, including the production of coesite, further evidence that the continental crust can dive to about 100km Depth and rapid reentry into the crust so that one of the high pressure signs preserved.