Atlas of Mylonites- and related microstructures

Mylonites form in response to high rates of strain within deep ductile shear zones, which are the extensions at depth of surface faults, thrusts and fault breccias. They can have many different mineralogical compositions and are therefore defined by their textural appearance. This atlas provides hig...

Πλήρης περιγραφή

Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς: Trouw, Rudolph A. J. (Συγγραφέας), Passchier, Cees W. (Συγγραφέας), Wiersma, Dirk J. (Συγγραφέας)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 2009.
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
Πίνακας περιεχομένων:
  • Cataclasites
  • Pseudotachylytes
  • Low-Grade Mylonites
  • Medium-Grade Mylonites
  • High-Grade Mylonites
  • Protomylonite, Mylonite and Ultramylonite
  • Mylonites Derived From Parent Rocks Other Than Granites and Gneisses
  • Shear Sense Indicators
  • Crystal-Plastic Deformation, Recovery and Recrystallisation of Quartz
  • “False” mylonites
  • Exercises.