Since the beginning of the 1980s, when Mandelbrot observed that earthquakes occur on ‘fractal’ self-similar sets, many studies have investigated the dynamical mechanisms that lead to self-similarities in the earthquake process. Interpreting seismicity as a self-similar process is undoubtedly convenient to bypass the physical complexities related to the actual process. Self-similar processes are indeed invariant under suitable scaling of space and time.
Original Source [2]
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Links:
[1] http://admin.indiaenvironmentportal.org.in/feature-article/long-range-dependence-earthquake-moment-release-and-implications-earthquake
[2] https://www.nature.com/articles/s41598-018-23709-4
[3] http://admin.indiaenvironmentportal.org.in/category/author/simone-barani
[4] http://admin.indiaenvironmentportal.org.in/category/author/claudia-mascandola
[5] http://admin.indiaenvironmentportal.org.in/category/author/eva-riccomagno-et-al
[6] http://admin.indiaenvironmentportal.org.in/category/journal/scientific-reports
[7] http://admin.indiaenvironmentportal.org.in/category/thesaurus/earthquakes
[8] http://admin.indiaenvironmentportal.org.in/category/thesaurus/geology
[9] http://admin.indiaenvironmentportal.org.in/category/thesaurus/natural-disasters
[10] http://admin.indiaenvironmentportal.org.in/category/thesaurus/italy
