A NUMERICAL STUDY ON LOCALIZED VOLUME REDUCTION IN ELASTIC MEDIA: SOME INSIGHTS ON THE MECHANICS OF ANTICRACKS

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dc.contributor.author Katsman R.
dc.contributor.author Aharonov E.
dc.contributor.author Scher H.
dc.date.accessioned 2025-02-16T08:50:24Z
dc.date.available 2025-02-16T08:50:24Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=31389698
dc.identifier.citation Journal of Geophysical Research: Solid Earth, 2006, 111, 3, B03204
dc.identifier.issn 2169-9313
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/47991
dc.description.abstract Porous rocks, subjected to compressive stress, often undergo mechanical compaction via grain crush and grain rearrangement, and chemical compaction by pressure solution. Such volume reduction processes are known to spontaneously localize under certain conditions, creating compaction and compacting shear bands, solution seams, and stylolites. However, the localization process is poorly understood. The formation and propagation of compaction bands have recently been studied using an elastoplastic spring network model (Katsman et al., 2005). In this paper, the same technique was employed to systematically analyze localized volume reduction (LVR) defects and their interactions with the surrounding elastic media, i.e., the stress distribution around an LVR region. Simulation results show that LVR regions experience stress concentrations at their tips,'reminiscent of mode I cracks. However, aside from this similarity point, comparison of stress around LVR regions to stress around cracks reveals that the stress/strain distribution in such LVR defects is quite different than that surrounding mode I cracks. Implications for stylolites and compaction band are thoroughly discussed. Copyright 2006 by the American Geophysical Union.
dc.title A NUMERICAL STUDY ON LOCALIZED VOLUME REDUCTION IN ELASTIC MEDIA: SOME INSIGHTS ON THE MECHANICS OF ANTICRACKS
dc.type Статья
dc.identifier.doi 10.1029/2004JB003607


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