Sedimentary Rayleigh waves across the Gangetic basin- A preliminary study
DOI:
https://doi.org/10.54302/mausam.v18i2.4451Abstract
Rayleigh wave dispersion in range of periods of 5 to 15 seconds from a number of earthquakes has been studied for paths crossing the Gangetic basin. The results have been compared with theoretical models, mostly with a single layer. They indicate the variation of the depth of the low velocity sediments from one path to another within the basin.
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