Characteristics of horizontal crustal movement in Weihe basin and adjacent zones by GPS observation

Based on the GPS data provided by CMONOC during 1999-2002 and observed by Seismological Bureau of Shaanxi Province during 2001-2002, we have obtained the crustal movement velocity field in Weihe basin and adjacent regions. The results show that the motion velocity in Weihe basin and adjacent zones i...

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Published in:Earthquake science 2004-05, Vol.17 (3), p.282
Main Authors: Dai, Wang-qiang, Ren, Jun, Zhao, Xiao-mao, Shao, Hui-cheng, Zhu, Gui-zhi
Format: Article
Language:English
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Average velocity
Earthquakes
Global positioning systems
GPS
Seismic activity
Velocity
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creator Dai, Wang-qiang
Ren, Jun
Zhao, Xiao-mao
Shao, Hui-cheng
Zhu, Gui-zhi
description Based on the GPS data provided by CMONOC during 1999-2002 and observed by Seismological Bureau of Shaanxi Province during 2001-2002, we have obtained the crustal movement velocity field in Weihe basin and adjacent regions. The results show that the motion velocity in Weihe basin and adjacent zones is characterized by distinct NE-directional stripped variation. The south border of Ordos block seems to show an discontinuous anti-clockwise rotation on the whole with an average velocity of about 5.7 mm·a^sup -1^ relative to Yulin site on the Ordos block. There is a left-lateral shear belt on both sides of Binxian-Xi'an-Lantian zone in the central Weihe basin, and its northern area has a better corresponding relationship with the dense zone of small earthquakes in Tong-chuan-Jingyang-Lintong-Weinan.[PUBLICATION ABSTRACT]
doi_str_mv 10.1007/s11589-004-0050-0
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subjects Average velocity
Earthquakes
Global positioning systems
GPS
Seismic activity
Velocity
title Characteristics of horizontal crustal movement in Weihe basin and adjacent zones by GPS observation
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