FRACTAL PROPERTIES OF MULTIPLE FRACTURE PATTERNS

dc.contributor.authorBotvina L.R.
dc.contributor.authorTyutin M.R.
dc.date.accessioned2026-05-27T18:13:11Z
dc.date.issued2007
dc.description.abstractThe power law describing the distribution of faults in the Earth’s crust found by many researchers confirms self-similarity of the pattern of discontinuities at the global level of development of the process of multiple fractures. The tangent of the inclination angle of these cumulative distributions was accepted in as the fractal dimension (D).
dc.identifierhttps://elibrary.ru/item.asp?id=15292784
dc.identifier.citationDoklady Earth Sciences, 2007, 417, 2, 1362-1365
dc.identifier.doi10.1134/S1028334X07090152
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/52936
dc.titleFRACTAL PROPERTIES OF MULTIPLE FRACTURE PATTERNS
dc.typeСтатья

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