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温都尔庙群分布于内蒙古集二线朱日和地区,西起五一台,向东经温都尔庙、汗白庙到白音诺尔、图林凯一带。 自1975年内蒙古区测队在这里发现蓝闪石以来,内蒙古地质局实验室,天津地质矿产研究所和河北地质学院在这里进行过大量研究工作,发现了迪尔石,铁滑石,黑硬绿泥石等矿物。1981年,笔者在这里工作,又发现了硬柱石,多硅白云母和文石等矿物。至此,温都尔庙群中已发现较完整的高压低温变质矿物组合,为研究和确定中朝陆台北侧早古生代板块俯冲带提供了矿物学资料。
Wendu Er temple groups located in Inner Mongolia set second-line Zhu Ri and the region, west of 51 units, eastward by the Wendu Er Temple, Khan White Temple to Baiyinnuoer, Turing Kai area. Inner Mongolia Geological Survey team since 1975 found in the blue amphibole, Inner Mongolia Bureau of Geology, Tianjin Institute of Geology and Mineral Resources and Geological Institute of Hebei conducted a lot of research here, found that the stone, iron steatite, black hard green Mud and other minerals. In 1981, I work here, but also found the hard stone, polycrystalline muscovite and aragonite and other minerals. Up to this point, more complete assemblages of high-pressure and low-temperature metamorphic minerals have been found in the Wenduermiao group, which provide mineralogical data for the study and determination of the Paleozoic plate subduction zone in the North side of the North-South China-North Korea.