The lacustrine carbonate rocks occur on a wide range of scales in the Palaogene and Neogene strata in the Hoh Xil Basin, Qinghai, and constitute an important part of the Miocene Wudaoliang Group sediments.

• 摘要湖相碳酸盐岩在可可西里盆地的古、新近纪地层中分布广泛，更是中新统五道梁群沉积的主要组成部分。