Geometric and kinematic analysis of a transpression terrane boundary: Minas fault system, Nova Scotia, Canada
The Minas fault system is an ENE-WSW trending transpressional boundary between the Appalachian Meguma and Avalon tectono-stratigraphic terranes of Nova Scotia, Canada. Along this boundary there is large-scale partitioning of deformation into distinct external (contractional) and internal (shear) zon...
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Published in | Flow Processes in Faults and Shear Zones Vol. 224; no. 1; pp. 201 - 214 |
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Main Authors | , |
Format | Book Chapter Journal Article |
Language | English |
Published |
The Geological Society of London
2004
The Geological Society, London Geological Society of London |
Series | Geological Society, London, Special Publications |
Subjects | |
Online Access | Get full text |
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Table of Contents:
- 13.1 Minas Fault System; Framework 13.2 Fault Rocks 13.3 Structural Elements and Geometric Relationships 13.4 Fault Zone Kinematics 13.5 Fault Zone Deformation Mechanisms 13.6 Strain Partitioning and Localization 13.7 Conclusion References