The Progressive Evolution of the Champlain Thrust Fault Zone: Insights from a Structural Analysis of its Architecture
Near Burlington, Vermont, the Champlain Thrust fault placed massive Cambrian dolostones over calcareous shales of Ordovician age during the Ordovician Taconic Orogeny. Although the Champlain Thrust has been studied previously throughout the Champlain Valley, the architecture and structural evolution...
| Main Author: | |
|---|---|
| Format: | Others |
| Language: | en |
| Published: |
ScholarWorks @ UVM
2018
|
| Subjects: | |
| Online Access: | https://scholarworks.uvm.edu/graddis/896 https://scholarworks.uvm.edu/cgi/viewcontent.cgi?article=1896&context=graddis |