Based on an analysis of the conodont biofacies, it is inferred that there was probably a deep-sea basin facies sedimentary environment in the Wenguer area during the early Middle Permian.
通过牙形石生物相分析,推断温古尔地区中二叠世早期可能为盆地相较深水沉积环境。
2
The sedimentation environment transformed from the fluvial and lake facies to the shallow seafacies, and finally to the deepseafacies.