Land subsidence pattern controlled by old alpine basement faults in the Kashmar Valley, northeast Iran: Results from InSAR and levelling
Fluid storage systems, such as oil, gas, magma or water reservoirs, are often controlled by the host rock structure and faulted terrain. In sedimentary basins, where no direct information about underlying structure is available, the pattern of ground deformation may allow us to assess the buried fau...
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Veröffentlicht in: | Geophysical journal international 2008-07, Vol.174 (1), p.287-294 |
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Sprache: | eng |
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