Fault and fracture reactivation in the Penola Trough, Otway Basin
This item is only available electronically. The Penola Trough, onshore Otway Basin, is a failed rift structure trending NW-SE on the South Australian-Victorian border. Following its formation during the Late Jurassic, the trough has been subjected to alternating periods of extension and compression,...
Main Author: | |
---|---|
Other Authors: | |
Format: | Thesis |
Language: | English |
Published: |
2012
|
Subjects: | |
Online Access: | http://hdl.handle.net/2440/92220 |