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...

Ful tanımlama

Kaydedildi:
Detaylı Bibliyografya
Asıl Yazarlar: Berend A. Verberne, Oliver Plümper, Christopher J. Spiers
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: MDPI AG 2019-05-01
Seri Bilgileri:Minerals
Konular:
nanograins
principal slip zone
crystallographic preferred orientation
amorphization
mirror-slip surface
faults
earthquakes
localization
Online Erişim:https://www.mdpi.com/2075-163X/9/6/328
Etiketler: Etiketle
Etiket eklenmemiş, İlk siz ekleyin!

Benzer Materyaller