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1)  Bayan Har
巴颜喀拉
1.
Sedimentary characteristics of the Bayan Har remnant ocean basin, northwestern China.;
巴颜喀拉残留洋盆的沉积特征
2.
Sedimentary facies and palaeogeography of the Triassic sedimentary basins in the Bayan Har mountainous area:an example from the Aba Zoige Basin,Sichuan;
巴颜喀拉三叠纪沉积盆地岩相与古地理——以阿坝-若尔盖盆地为例
3.
The Hoh Xil-Bayan Har sedimentary basin where the active Triassic widely dis-tributed and adjacent paleocontinent where the stable Triassic spreaded had been TriassicTethys sea area.
可可西里一巴颜喀拉活动型三叠系,与相邻古陆上的稳定型三叠系分布区,构成特提期三叠纪海域。
2)  Bayan Har Mountains
巴颜喀拉山
1.
Thermochronology of the uplift of the Bayan Har Mountains, Qinghai, China;
青海巴颜喀拉山隆升的热年代学研究
2.
The Floristic Characteristics in the Region of Bayan Har Mountains;
巴颜喀拉山地区植物区系研究
3)  western segment of the Bayan Har Mountains
巴颜喀拉山西段
1.
Discovery of a Permian paleo-seamount in the western segment of the Bayan Har Mountains, China and its significance;
巴颜喀拉山西段二叠纪古海山的发现及意义
4)  Bayankala folded belt
巴颜喀拉褶皱带
1.
Up to now,no paleomagnetic data has been reported on the Bayankala folded belt,which is an upside-down triangle area located among the Yangze,North China,Tarim,and Qiangtang-Changdu blocks.
迄今为止,位于扬子地块的西北缘,夹持于扬子、华北、塔里木和羌塘—昌都地块之间呈倒三角形构造区块的巴颜喀拉褶皱带尚未有构造古地磁研究成果报导。
5)  eastern part of Bayan Har Mountains
巴颜喀拉山东段
6)  Bayanharshan Group
巴颜喀拉山群
1.
The Bayanharshan Group with a great thickness, unvarying lithology, and few body fossils outcrops widely in the Qumarleb-Zhidoi area, southern Qinghai.
青海南部曲麻莱—治多地区广泛出露厚度巨大、岩性单一、实体化石稀少的三叠系巴颜喀拉山群,其地层划分与对比因缺乏明显标志而相对困难。
2.
Trace fossils from the upper pant of the Bayanharshan Group (Upper Triassic) in Qumarleb-Zhidoi area, Southern Qinghai Province, have been systematically gathered for the first time, they comprise 54 ichnospecies in 33 ichnogenera.
首次对青海南部曲麻莱-治多地区巴颜喀拉山群上部(上三叠统)遗迹化石进行了系统采集,共采获遗迹化石33属54种。
补充资料:巴颜喀拉山脉
在青海省东南部。昆仑山脉东段的南支。长江和黄河的分水岭。除个别山峰外,海拔在5000米以下。同名主峰海拔5267米。山麓为良好牧场。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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