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中文摘要：
利用2001~2004年关中地区及周边区域GPS观测资料,运用整体旋转与线性应变模型（RELSM）研究了关中地区地壳水平运动及应变场特征,探讨了其与地震、地裂缝活动的关系。结果表明：彬县—西安—蓝田是关中地区地壳水平差异运动的分界带;泾阳—西安—咸阳—临潼—三原地区同时是最大剪应变、面膨胀高值区,也是地壳运动显著差异带,同时该区还发育多条深大活动断裂,具备发生中强地震的必要条件;甘青块体的向东挤压加之周围块体的运动,形成了关中地区西部表现为压缩,而东部表现为伸展的特点;泾阳—西安—咸阳地区地壳伸展运动强烈,地裂缝十分发育。
英文摘要：
Using the GPS data of Guanzhong and around area during 2001~2004,the author used the model with rotation in the entire block and linear strain,analyzed the crustal horizontal deformation-strain features of the aforementioned area.The relations between earthquakes or ground fissure and the crustal horizontal movement as well as stain distribution features of this area were also discussed.
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