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...
Κύριοι συγγραφείς: | , , |
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Συγγραφή απο Οργανισμό/Αρχή: | |
Μορφή: | Ηλεκτρονική πηγή Ηλ. βιβλίο |
Γλώσσα: | English |
Έκδοση: |
Berlin, Heidelberg :
Springer Berlin Heidelberg : Imprint: Springer,
2009.
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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.