The geological evolution and mineralised environments of the Tasman Geosyncline

Title: The geological evolution and mineralised environments of the Tasman Geosyncline
Creator: Pelham, D A
Subject: Geosynclines -- Tasmania
Subject: Geology -- Tasmania
Subject: Ore deposits -- Tasmania
Subject: Mineralogy -- Tasmania
Date: 1983
Date: 2013-04-03
Type: Thesis
Type: Masters
Type: MSc
Identifier: vital:5030
Identifier: http://hdl.handle.net/10962/d1006936
Identifier: Geosynclines -- Tasmania
Identifier: Geology -- Tasmania
Identifier: Ore deposits -- Tasmania
Identifier: Mineralogy -- Tasmania
Description: From introduction: The Tasman Geosyncline covers the eastern part of the continent of Australia, an area of over 2 million km'. The area has been a major source of Australian gold and tin production, and though it contains important base metal sulphide deposits, these are overshadowed in scale by the very large stratabound Proterozoic deposits (for example, Mt Isa, Broken Hill and McArthur River). This dissertation deals with the metallic mineral deposits of the Tasman Geosyncline, and as such does not include the extensive post Palaeozoic continental successions, with their important coal reserves, that overlie the deformed geosyncl i nal sequences.
Format: 202 p., pdf
Publisher: Rhodes University, Faculty of Science, Geology
Language: English
Rights: Pelham, D.A.

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