The well-known gravity flow sediments were formed by the debris, slide and turbidity flows in the Late Jurassic-Early Cretaceous in Shalagang mining area of Jomzi Basin in southern Tibet, which consisted of the slope elastic rocks and interbeds of siliceo
The well-known gravity flow sediments were formed by the debris, slide and turbidity flows in the Late Jurassic-Early Cretaceous in Shalagang mining area of Jomzi Basin in southern Tibet, which consisted of the slope elastic rocks and interbeds of siliceo
摘要西藏南部江孜盆地的沙拉岗矿区发育一套晚侏罗世至早白垩世的碎屑流、滑动流与浊流等重力流沈积，主要由斜坡相碎屑岩夹矽质岩和灰岩构成。