Abstract
On the basis of the velocity field results of horizontal crustal movement obtained from GPS measurements during the periods of 1993–1999, 1999–2001 and 2001–2003 in the northeastern margin of Qinghai-**zang block, and by the inversion of negative dislocation model for the elastic block boundaries, we provide in this paper a qualitative analysis and quantitative description for the difference of motion and deformation between the tectonic blocks and their boundary faults, time-space distribution of tectonic strain field, and locations with highly accumulated strain energy and correlative intensity. Furthermore, taking the regional tectonics and block strain into full consideration, we investigate the common features of background precursors relating to location prediction for M>-6 earthquakes.
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Foundation item: Joint Seismological Science Foundation (603001) and Project of China Earthquake Administration during the tenth five-year (100501-04).
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Zhang, X., Jiang, Zs., Wang, Q. et al. Inversion for negative dislocation on elastic block boundaries in the northeastern margin of Qinghai-**zang block and prediction for strong earthquake location. Acta Seimol. Sin. 18, 666–677 (2005). https://doi.org/10.1007/s11589-005-0094-9
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DOI: https://doi.org/10.1007/s11589-005-0094-9
Key words
- elastic block boundary
- negative dislocation model
- horizontal crustal movement
- inversion
- study of earthquake examples