摘要
利用1998—2008年北天山地区近30个站的GPS观测资料,获取了研究区内现今地壳运动速度场和主要断层的活动速率。GPS运动速率表明:北天山地区的南北向地壳缩短表现为非均匀性,速度吸收的差异性表现出与该地区地震发生频度有一定的相关性;GPS测量得到的现今断裂总体活动特征与地质学推断结果一致,但量值存在差异。
Using GPS measurements in the Northern Tienshan Mountains from 1998 to 2008,we obtain the present-day crustal movement velocity field for more than 30 sites,at the same time,estimate active rates on the major faults in the studied region.The GPS velocity results show that there is non-uniformity for N-S direction crustal shortening of northern Tianshan area and it shows the correlation between the differences of the absorption rate and frequency of the earthquake occurring.The active faults movement characters derived from the GPS measurement results are consistent with the geological results,but there are differences in the value.
出处
《大地测量与地球动力学》
CSCD
北大核心
2010年第6期1-5,共5页
Journal of Geodesy and Geodynamics
基金
国家科技支撑计划(2008BAC35B04-5)
地震科学联合基金(A08056)
新疆维吾尔自治区科学研究和技术开发(含攻关)项目(200741121)
国家自然科学基金(D0408)
关键词
北天山地区
活动构造
断层运动
GPS测量
地壳变形
northern Tianshan region
active tectonics
fault movement
GPS measurement
crustal deformation