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dc.contributor.author Chen Z.
dc.contributor.author Bai W.
dc.date.accessioned 2025-02-08T08:30:03Z
dc.date.available 2025-02-08T08:30:03Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=31308985
dc.identifier.citation Geophysical Journal International, 2006, 165, 1, 272-278
dc.identifier.issn 0956-540X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/47892
dc.description.abstract A fault model is used to analyse creep growth process of microcracks in damage zone near the tips of fault by means of the rheology fracture mechanics. When microcracks in the zone link each other and their deformation quickly intensifies, it means that an earthquake is taking place to a certain degree. The relationships among some key parameters that are correlated to the growth of microcracks are analysed theoretically. These parameters include failure time of fault, number of microcracks in unit area, stresses field, yield strength and rheological properties of medium. The results indicate that the model proposed here is reasonable to describe the pregnant process of an earthquake. In the meantime, this research shows that, with the results of in situ surveys and lab experiments, it is possible to estimate the time span for a fault expanding. © 2006 The Authors Journal compilation © 2006 RAS.
dc.subject CREEP
dc.subject EARTHQUAKE
dc.subject FAULT
dc.subject GROWTH
dc.subject MICROCRACK
dc.subject MODEL
dc.title FAULT CREEP GROWTH MODEL AND ITS RELATIONSHIP WITH OCCURRENCE OF EARTHQUAKES
dc.type Статья
dc.identifier.doi 10.1111/j.1365-246X.2006.02890.x


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