1) Qinghai-Xizang subplate
青-藏亚板块
2) Qinghai-Tibet Subplate
青藏亚板块
1.
Spatio-temporal Evolution Characteristics of Strong Earthquakes in Qinghai-Tibet Subplate;
青藏亚板块强震时空演化特征研究
3) The Qinghai-Tibet plate
青藏板块
1.
The Qinghai-Tibet plate is characterized by strong activity due to the recent orogeny.
从青藏板块中发现的石炭纪含砾冰水沉积与桉属植物群的分布对比研究,认为青藏板块仍属南大陆范畴。
4) Qinghai-Tibet plateau
青藏块体
1.
In order to monitor and research crustal movement and deformation in northeast margin of Qinghai-Tibet Plateau and their relationship with strong earthquake activity, a reexamination of GPS (C) Net in Hexi region was carried out in 1999.
利用青藏块体东北缘地区 1993与 1999年GPS观测获得的地壳水平运动速度场结果 ,初步研究了该区的应变场与构造变形。
5) Qinghai-Tibet block
青藏块体
1.
Preliminary study on the relativity between the strong earthquake in Qinghai-Tibet block and moderate strong earthquake in Qilian mountain seismic belt;
青藏块体强震与祁连山地震带中强震相关性的初步探讨
2.
Based on the data of leveling across faults in northeast margin area of Qinghai-Tibet block,the statistics,comparison,analysis and study are made on three aspects as follows: the spatial distribution of abnormal fault deformation,the average rate of fault movement in different belt,and the distribution of group abnormal fault deformation in time dimension.
根据青藏块体东北缘地区的跨断层流动水准测量资料,分别从断层形变异常的空间分布特征,不同断裂带上断层形变平均活动速率的分布和断层形变群体性异常在时间上的分布三个方面进行了统计、对比、分析和研究。
6) Qinghai-Xizang block
青藏块体
1.
Anomalous fault activity along the boundary of Qinghai-Xizang block before the kunlunshankou earthquake with M=8.1;
昆仑山口西8.1级地震前青藏块体边界断层异常活动
2.
HTThe distribution of velocity field of crustal horizontal movement and apparent strain field in the northeast margin of Qinghai-Xizang block is studied on the basis of GPS data in 1993 and 1999.
利用青藏块体东北缘地区 1 993、1 999年GPS观测资料 ,给出了本区地壳水平运动速度场及视应变场分布图 ,提出了由位移观测值直接求解块体旋转和变形参数的方法 ,初步研究了本区构造块体运动与变形特征 。
补充资料:柳梢青 藏头
【诗文】:
轮不催生灭。焰里莲开五叶。得金花,成芝草,分无阙。生马钰愚人,然悟家缘痛切。劈恩山,明千古,谈心月。
【注释】:
【出处】:
轮不催生灭。焰里莲开五叶。得金花,成芝草,分无阙。生马钰愚人,然悟家缘痛切。劈恩山,明千古,谈心月。
【注释】:
【出处】:
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