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- W2377590086 abstract "There are two earthquakes in Gaize on Jan 9(MS 6.9)and Jan 16,2008(MS 6.0).The two earthquakes were selected as examples to obtain the co-seismic deformation field with the 2-pass differential interferometric processing method.The results show that the earthquake faults locate near the tip of the Yibuchaka-Riganpeicuo Fault,and both seismic faults are normal faults;The seismogenic fault of the main shock strikes about N30°E and that of the aftershock strikes about N21°E;There is evidence of surface rupture along the mainshock's causative fault,but no surface rupture has been observed on the aftershock fault;The co-seismic deformation field is about 30km in length and 20km in width;The maximum displacement in LOS of the hanging wall of the main-shock fault is 39.2cm,and that of footwall is 11.2cm,the relative dislocation between them is 50.4cm;The displacement caused by the aftershock is 9.4cm(LOS)." @default.
- W2377590086 created "2016-06-24" @default.
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- W2377590086 date "2009-01-01" @default.
- W2377590086 modified "2023-09-24" @default.
- W2377590086 title "OBSERVING COSEISMIC DEFORMATION OF THE GAIZE,XIZANG EARTHQUAKE WITH DIFFERENTIAL INTERFEROMETRIC SAR" @default.
- W2377590086 hasPublicationYear "2009" @default.
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