Formation of flower structures in a geological layer at a strike-slip displacement in the basement


статья в журнале
Авторы: Stefanov Y.P.   (ИНГГ СО РАН)   Bakeev R.A.    
дата публикации: 2015
реферат:
Formation of dislocations in a geological layer at a strike-slip displacement in its basement is studied by three-dimensional (3D) numerical modeling. It is shown that the pattern of strain localization is determined by the initial stress state or thickness of the deformed layer as well as by the Poisson ratio and strength of the medium. Three types of fracture zones are observed. Shear bands of the first type are dominated by the propeller-like surfaces of Riedel R-shears, which merge into a single main fault with feathering structures
первоисточник: Izvestiya. Physics of the Solid Earth
том: 4
страницы: 535-547
ISBN:
ISSN:
внешние ссылки:
WoS   WoS (цитирование)
DOI  
РИНЦ SPIN  
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полный текст статьи

pse-2015-04-535