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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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Sonraí Bibleagrafaíochta
Main Authors: Berend A. Verberne, Oliver Plümper, Christopher J. Spiers
Formáid: Artigo
Teanga:Inglês
Foilsithe: MDPI AG 2019-05-01
Sraith:Minerals
Ábhair:
Rochtain Ar Líne:https://www.mdpi.com/2075-163X/9/6/328
Clibeanna: Cuir Clib Leis
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