1) the north block of Tibet Plateau
青藏北块
1.
Since 1700,M≥7strong earthquakes have had an obvious commensurability and orderliness in the north block of Tibet Plateau.
自1700年以来,青藏北块地区M≥7强震具有显著的有序性,其主要有序值为53～54a,26～27a,11～12a与3～4a等。
2) northeastern margin of Qinghai-Tibet block
青藏块体东北缘
1.
By use of horizontal velocity data observed by GPS during 2001—2004 and 2004—2007 in the northeastern margin of Qinghai-Tibet block,aided by the negative dislocation model,the characteristics of horizontal crustal movement and the status of strain accumulation of this area are researched and following conclusion are drawn.
利用青藏块体东北缘2001—2004年、2004—2007年GPS水平运动速度场结果,借助负位错模型,研究该区当前的地壳水平运动特征与应变积累状况。
3) the northeastern margin of Qinghai-Tibet block
青藏块体东北缘
1.
By transforming the reference frame of the velocity field of horizontal movement observed by GPS during 1999-2001 and 2001-2004 in the northeastern margin of Qinghai-Tibet block and then deducting the holistic movement of the region from it,the result out velocity field reflecting relative movement in the region is gotten.
将1999～2001年、2001～2004年两个时段中青藏块体东北缘GPS水平速度场进行参考框架的变换,扣除区域刚性整体平移和旋转,得到反映区域内部相对运动的水平速度场。
4) northern block of Qinghai-Tibet Plateau
青藏高原北块
5) Northeastern Qinghai-Xizang block
青藏块体东北部
6) the north of Qinghai-Xizang block
青藏块体北部
补充资料：东北人民自卫军(见东北军区)
东北人民自卫军(见东北军区)
Northeast People's Self-Defense Army
黔勺eLR望份驴we衬un不月L八比曰卫乐(Northeast PeoPle’ssel卜DefenseA肋y)见东北军区。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条