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GPS测量揭示的福建沿海地区的现今地形变
引用本文:郭逢英,史粦华,丁学仁,林继华,刘序俨,黄声明,黄立人,马青.GPS测量揭示的福建沿海地区的现今地形变[J].大地测量与地球动力学,2003,23(3):87-92.
作者姓名:郭逢英  史粦华  丁学仁  林继华  刘序俨  黄声明  黄立人  马青
作者单位:1. 福建省地震局,福州,350001
2. 中国地震局第一地形变监测中心,天津,300180
基金项目:福建省计委“九五”科技攻关项目,福建省地震局 10 5 -0 4A课题,国家重大科学工程“中国地壳运动观测网络”项目
摘    要:根据福建GPS监测网3期(1997,1999,2001)观测资料的计算结果,分析了福建沿海地区的现今地形变特征。(1)福建地区有两个剪应变相对集中区,北部是湾口、闽清一带;南部是泉州、厦门一带。这两个区的剪应变随时间变化有加强的趋势。(2)南部剪应变集中区基本处于压应变环境,并且主要断裂两侧存在相对较高的剪应变集中区,值得关注。

关 键 词:GPS  福建沿海地区  现今地形变  位移场  应变场  剪应变
文章编号:1671-5942(2003)03-0087-06
修稿时间:2003年5月6日

CRUSTAL DEFORMATION ALONG COAST OF FUJIAN REVEALED BY GPS
Guo Fengying,Shi Linhua,Ding Xueren,Lin Jihua Liu Xuyan,Huang Shengming,Huang Liren and Ma Qing Seismological Bureau of Fujian Province,Fuzhou\ No. Crustal Deformation Monitoring Center,CSB,Tianjin\.CRUSTAL DEFORMATION ALONG COAST OF FUJIAN REVEALED BY GPS[J].Journal of Geodesy and Geodynamics,2003,23(3):87-92.
Authors:Guo Fengying  Shi Linhua  Ding Xueren  Lin Jihua Liu Xuyan  Huang Shengming  Huang Liren and Ma Qing Seismological Bureau of Fujian Province  Fuzhou\ No Crustal Deformation Monitoring Center  CSB  Tianjin\
Institution:Guo Fengying,Shi Linhua,Ding Xueren,Lin Jihua Liu Xuyan,Huang Shengming,Huang Liren and Ma Qing 1) Seismological Bureau of Fujian Province,Fuzhou\ 350001 2) No.1 Crustal Deformation Monitoring Center,CSB,Tianjin\ 300180
Abstract:In the light of the computed results of measurement data of GPS observation network in 3 periods (1997, 1999, 2001)we have analyzed the current deformation characteristics along the coast of Fujian as follows. (1) There are two relative concentration areas of shear strain in Fujian:the northern one is Wankou-Minqing and the southern one is Quanzhou-Xiamen.In addition,the shear strains in the two areas show a increasing trend with time. (2)the southern area of shear strain concentration is basically in a compressive strain condition and there exists relative high shear strain concentration area on the two sides of the principal fault.
Keywords:coastal area of Fujian  displacement field  strain field  shear strain
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