摘要
联合福建省近几年福清、泉州综合场地GPS观测数据和水准复测数据,分析了两个跨断层综合场地的三维运动特征。结果显示:16个综合场地GPS测站相对华南块体的无整体旋转速率约为5mm/a,方向为北东向和北西向。长乐-诏安断裂带的三组次级断裂均存在走滑运动,长乐-诏安断裂带以压性活动为主,且福建地区地块形变具有南强北弱的特征。
High precision GPS and leveling data of recent years are used to estimate 3D velocities of fault zones in Fuqing and Quanzhou of Fujian area.The results are as follows:Velocities of 16 GPS stations in Fuqing and Quanzhou exhibit northeastward or northwestward movement,and the value is are about 5mm/a relative to the NNR on crustal motion of Southern China block.The three secondary faults of Changle-Zhaoan fault show slip motion and compressive activities,and the activity of north segment is weaker than that of the south segment in Fujian area.
出处
《全球定位系统》
CSCD
2016年第3期93-96,共4页
Gnss World of China
基金
福建省地震局科研基金(编号:SF201201
Y201501)
关键词
GPS
水准
无整体旋转
基线
高程
GPS
leveling
NNR reference frame
baseline
elevation