Abstract.
The geographical scope of the experiment in this paper is Dangxiong in Tibet. The rift basin of Yangbajing-Dangxiong-Gulu locates at the east side of the Nyainqentanglha. The crustal activities in Dangxiong basin are frequent and a great deal of geothermal energy converged under the surface. The geothermic resources were used through the exploitation of underground water. The excessive extraction caused the surface deformation in surrounding areas of the pump wells. In this paper, we investigate the surface deformation caused by the geothermal extraction in Dangxiong with 23 Envisat ASAR images from 2006 to 2010 based on the time series analysis. The results show that the center of the basin was relatively stable. The deformation rate was between -1 mm/yr and 2 mm/yr. The surface subsidence rate of the region with the pump wells was about 8 mm/yr.
© 2012 by Walter de Gruyter Berlin Boston
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- Masthead
- Editorial: Special Issue on Deformation Monitoring
- Model selection for system identification by means of artificial neural networks
- Adjustment of highly non-linear redundant systems of equations using a numerical, topology-based approach
- Optimized Kalman filter versus rigorous method in deformation analysis
- The application of the model of coordinate S-transformation for stability analysis of datum points in high-precision GPS deformation monitoring networks
- Velocity estimation of GPS base stations considering the coloured noises
- Spectral analysis of structural deformation – A case study
- Ambient vibration monitoring of slender structures by microwave interferometer remote sensing
- A 3-d laser scanning system and scan data processing method for the monitoring of tunnel deformations
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- Point-based and plane-based deformation monitoring of indoor environments using terrestrial laser scanners
- Recurring mass movements on the Danube's bank at Dunaszekcső (Hungary) observed by geodetic methods
- Monitoring ground subsidence in Shanghai maglev area using two kinds of SAR data
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