Nanocrystalline Principal Slip Zones and Their Role in Controlling Crustal Fault Rheology

Principal slip zones (PSZs) are narrow (<10 cm) bands of localized shear deformation that occur in the cores of upper-crustal fault zones where they accommodate the bulk of fault displacement. Natural and experimentally-formed PSZs consistently show the presence of nanocrystallites in the &am...

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Библиографические подробности
Главные авторы: Berend A. Verberne, Oliver Plümper, Christopher J. Spiers
Формат: Artigo
Язык:Inglês
Опубликовано: MDPI AG 2019-05-01
Серии:Minerals
Предметы:
nanograins
principal slip zone
crystallographic preferred orientation
amorphization
mirror-slip surface
faults
earthquakes
localization
Online-ссылка:https://www.mdpi.com/2075-163X/9/6/328
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