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西藏班戈一带地处著名的藏北湖区东部,海拔4500米以上。在构造上位于雅鲁藏布江深断裂带以北,班公湖一东巧一怒江深断裂的南侧,地层区划称岗底斯一念青唐古拉区班戈分区或奇林湖分区,包括班戈县以西,奇林湖以东,黑(河)阿(里)公路以南,果忙错一普嘎错以北、绵延于班戈湖盆地南北两侧、主要由白垩系组成的呈北西西一南东东方向延伸的边缘山地。盆地内多为第三系和第四系覆盖。按已往习惯,把班戈湖盆地南缘的郎瑞
Tibet Bangor area is located in the eastern part of the famous Lake in northern Tibet, elevation 4,500 meters above. Located in the north of the Brahmaputra deep fault zone to the north of Bangong Lake and on the south side of Bangong Lake to the east of Nujiang River, the stratigraphic division is called the Bangor or Qilin Lake subregion of Gangnam-Nyangtanggula, Gangbuk including west of Bangge County, To the east of Qilin Lake and to the south of Ah-Li (Heihe) Highway, north of Panga fault, where the fault is busy, it stretches in both north and south sides of the Bangor Lake Basin, and is mainly composed of Cretaceous northwest and south-east The eastern edge of the extension of the mountain. The basin is mostly Tertiary and Quaternary coverage. According to past habits, to the southern edge of the Bangor Lake Lang Rui