黄河的发源地在青海的巴颜喀拉山上。
The source of the Yellow River can be traced to the Bayankela Mountains of Qinghai Province.
巴颜喀拉山北麓古高位湖相沉积的形成时代可能为中更新世。
The forming age of the lacustrine sedimentation from ancient high level lake at the north foot of Mt. Bayankala could be middle Pleistocene epoch.
巴颜喀拉山脉南端位于四川省阿坝县、壤塘县与马尔康县交界地区。
The southern end of the Mts. Bayan Har lies in common boundary area of Aba, Zamtang and Barkam counties.
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.
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.
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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