Abstract
The Andaman–Sumatra is one of the seismically active subduction zones and experienced three largest earthquakes in the recent past and rupturing more than 1,600-km-long portion of the plate boundary. The seismicity analysis of these large earthquakes source region (5°S–15°N latitude and 90°E–103°E longitude) has been carried out by several researchers and quantified the spatial and temporal variation of b-value which is a proxy to differential stress conditions and fractal dimension which is an indicator of material heterogeneity and strength. The results of all these studies clearly bring out the low b-value and low fractal dimension corresponding to locales were sizable magnitude earthquakes have occurred. Further locales of high stress regions are identified.
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Srivastava, K., Rani, S. & Srinagesh, D. A review of b-value imaging and fractal dimension studies in the Andaman Sumatra subduction. Nat Hazards 77 (Suppl 1), 97–107 (2015). https://doi.org/10.1007/s11069-014-1143-2
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DOI: https://doi.org/10.1007/s11069-014-1143-2