2009/10/20 by Pathikrit Bhattacharya, Kamal Kamal, Bhattacharya, Pathikrit +3
Earth and Planetary Sciences · Physics and Astronomy · #Data Analysis #FOS: Physical sciences #Geological and Geochemical Analysis #Geophysics (physics.geo-ph) #High-pressure geophysics and materials #Statistics and Probability (physics.data-an) #earthquake and tectonic studies #physics.data-an #physics.geo-ph
paper · pdf · doi:10.48550/arxiv.0910.3738
24 pages, 7 figures, 3 tables
openalex publication_date 2009/10/20 · arxiv created 2009/10/28 · arxiv updated 2009/12/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/28
We have analyzed, for the first time, the time cumulant of magnitudes of an aftershock sequence since the mainshock. This comes out to be a remarkable straight line whose slope is characteristic of the fault zone. This will provide an useful tool in understanding the temporal distribution of aftershocks after a specific mainshock.