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,...

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Bibliographic Details
Main Author: Grosser, B. T.
Other Authors: School of Earth and Environmental Sciences
Format: Thesis
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/2440/92220