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Contrasted morphologies of the Western and Eastern Piedmonts of the Mt Lofty Ranges, South Australia
The Mt Lofty Ranges is a horst that evolved in two stages. The western margin developed as part of the South Australian Shatter Belt during the separation of Australia and Antarctica. Gulf St Vincent formed at this time. Though recurrently active the upland dates essentially from the Early Eocene with major uplift in the later Cenozoic. By contrast, the eastern faulted margin postdates the Middle …
Creator
- Twidale, Charles Rowland
- Bourne, Jennifer Anne
Publisher
- Ediciones Universidad de Salamanca (España)
Subject
- Geology
- Geology
- Geología
Type of item
- Artículo
- Article
Date
- 2016-07-21T09:04:09Z
- 2016-07-21T09:04:09Z
- 2014-12-15
- 2014-12-15
- 2016-07-21
- 2016-07-21
Creator
- Twidale, Charles Rowland
- Bourne, Jennifer Anne
Publisher
- Ediciones Universidad de Salamanca (España)
Subject
- Geology
- Geology
- Geología
Type of item
- Artículo
- Article
Date
- 2016-07-21T09:04:09Z
- 2016-07-21T09:04:09Z
- 2014-12-15
- 2014-12-15
- 2016-07-21
- 2016-07-21
Providing institution
Aggregator
Rights statement for the media in this item (unless otherwise specified)
- http://creativecommons.org/licenses/by-nc-nd/4.0/
Rights
- info:eu-repo/semantics/openAccess
Creation date
- 2016-07-21T09:04:09Z
- 2016-07-21
Identifier
- oai:gredos.usal.es:10366/129866
- Studia Geologica Salmanticensia, 49 (2013)
- 0211-8327
- http://hdl.handle.net/10366/129866
Format
- application/pdf
Language
- eng
Providing country
- Spain
Collection name
First time published on Europeana
- 2017-07-07T14:04:56.197Z
Last time updated from providing institution
- 2017-07-07T14:04:56.197Z