重建的地层层序和沉积地质特征显示巴颜喀拉盆地主体三叠系复理石沉积是周缘前陆盆地。

The stratigraphic sequences and sedimentological characteristics indicate that the main body of Bayan Har Basin is composed of Triassic flysch sediments deposited in a foreland basin during Triassic.

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在巴颜喀拉山群中采获早三叠世和晚三叠世诺利期双壳化石，查明了测区三叠纪巴颜喀拉山群最高层位为诺利期陆棚—海陆交互相沉积。

It is ascertained that the highest horizon of the Triassic Bayan Har Mountain Group in the survey area is Noric shelf-paralic deposits.

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